Master in England, in 2005 after returning committed to the promotion of cultural and creative industries is now a culture of the company CEOs. Published a series of planned introduction and widespread concern in the community works, such as the ((poor boy rich girl was raised with support "and" When the gentleman boys and girls to do lady, "" Bottle of Love and Marriage Age, "" from 1 to 00000 to 100 million - with a wealth of high-speed road you enter ", ((from 1 000 to 1 0000 to make you pay double the l 3-step" and imported from overseas copyright excellent book "Life reference", "Roaming Tales economic world: pig house money "and so.
Higher elevations, large areas of flat terrain smaller.
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No. 4
Loess Plateau
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No. 5
Heights. Han Yang Xiong, "Yu Fu Hunting": "emblem car light weapons, Hong Dongqie hunting, earnestly Zhen Zhen, Ling Yuan by Sakamoto, poor offerings were very far away, above the plateau phase and Lie exhale." Tang Wangwei "Pastoral Music "Poetry 5:" Smoke in far mountain villages, the horizon Tree Plateau. "
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The definition of the plateau
Altitude above 1,000 meters in general and vast, open terrain, to clear the steep slopes surrounding the sector, a relatively complete large area known as the plateau uplift. The main difference between the plateau and the plains are at higher elevations, it is a complete different from the large area of mountain uplift. Plateau known as "earth stage," said, it is a large area in the long-term continuous movement of crustal uplift formation. It is different from the high plains of the larger so, on the larger and smaller flat rolling surface is different from mountains. Some broad flat plateau surface, undulating terrain; some high principle of rolling hills, the terrain changed dramatically. The plateau is the world's highest Qinghai-Tibet Plateau of China, the largest plateau of the Antarctic ice plateau. Broad, flat upland, usually full of cliffs in all directions, but sometimes surrounded by mountains. The most essential features of the plateau is ︰ low-lying relative height above sea level is quite high. Distribution of a wide plateau, together with the basin surrounded with, which together account for about 45% of Earth's land surface. World's top ten plateau (altitude) Name average elevation (m) Area (square kilometers) the Pamirs Plateau 4500250 380035 400010 Ecuador, Bolivia, highland 30002 highland plateau 25,001,280 Antarctic ice plateau of Mexico the Ethiopian highlands 220045 200030 200035 Yunnan-Guizhou Plateau Greenland ice plateau of Armenia 200030 1900187 Plateau Plateau type Surface morphology at high altitude plateau can be divided in several categories: one is relatively flat top surface of the plateau, such as China's Inner Mongolian Plateau; one is the undulating ground, the top of the plateau is still quite broad, such as the Qinghai-Tibet Plateau of China; One is split plateau, such as China's Yunnan-Guizhou Plateau, water cutting deeper, ups and downs, the top surface was still wide. Loess Plateau is one of the four, most of the thick layer of loess plateau coverage. Strata exposed in the Loess Plateau complete topographic diversity, is the most typical loess areas of physical geography. Reflect the different types of highland origin of the plateau and its subsequent erosion of history. The most common is the construction of the plateau, much of Africa is such an uplift of the land mass, the Arabian Peninsula of the Deccan Plateau and the Indian subcontinent is the same terrain. Much smaller Plateau horst fault block and they are the fault system along the edge of the plateau uplift or _set_tlement adjacent to block some of the time continued to hold high. Horst usually easier to distinguish between a large fault block. Tilted fault block is a variation of this plateau has a relatively steep sloping sides and a bradycardia in the ground. Other types of rocky plateau by the solid. Spray a large area of volcanic basalt lava flows caused many plateau. If ︰ Northern Ireland Antrim (Antrim) basalt plateau, the northwestern United States Columbia - Snake River Basin, Ethiopia and northwestern India, the Deccan Plateau.
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The characteristics of the plateau
Plateau elevation, low air pressure, low oxygen content, using the low-pressure oxygen environment, physical strength and endurance can improve the quality of the human body, so the endurance sports world as the "treasure." The 19th Olympic Games in 1968 in the highland city of Mexico City, players from the African plateau, covering the Middle and Long Distance and Marathon, 5 and 5 runner-up titles, two third place. Since then, the Plateau has become the world sports Middle and Long Distance, marathon, race walking and other endurance training "treasure." Other highland areas receiving more solar radiation, sunshine time is long, very rich solar energy resources. Plateau is lower than the boiling point of water, 100 ℃, as with normal rice cooker to cook, then half-cooked. In the arid and arid areas, often leading to the cutting effect of plate-like terrain Xingcheng, especially if there is rock solid, then the top cover. This is typical of the southwestern U.S. border landscape, where the ground has been eroded as the original platform and to stack (smaller Pingdingshan). The topography of high altitude often causes its own unique local climate. In the Basin and Range terrain, height, together with the surrounding mountains with effect from the storm caused an effect, producing dry and semi-arid environment.
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The formation of the plateau
Ages generally flat plateau shorter, but long years due to the long-term weathering erosion, relatively low, but looks like the mountain. Appalachian eastern United States is actually the western end of this like a mountain plateau, or mesa. The formation of the Tibetan Plateau 240 million years ago, due to plate motion, separated from the Indian plate moving northward at a relatively high speed, extrusion, and its strong northern fault and fold uplift of the Kunlun Mountains and Hoh Xil region to promote Lung Health for the land, as India continue north into the plate under the ancient oceanic crust, and continue to promote the rupture of oceanic crust, about 2.1 billion years ago, re-entering the northern Tethys tectonic active, northern Qiangtang, Karakorum Mountains, Tanggula leaching out of the sea mountain range; to 80 million ago, before continuing northward drift of Indian plate, once again caused a strong tectonic movement. Gangdise Hill, Nyainqentanglha Mountain sharp rise in parts of northern Tibet and southern Tibet and also from the sea into land. Ease of spread throughout the terrain, rivers, lakes, clouds, there have been vast plains, humid climate, lush jungle. Plateau landscape shape. Geology on the rise during the plateau known as the Himalayan tectonic movement. Qinghai-Tibet Plateau uplift process is not uniform movement, not a one-time surge, but the increase has gone through several different stages. Have to uplift each time to the evolution of the plateau landscape. Ten thousand years ago, the plateau uplift is faster to increase the average speed of 7 cm per year, making it on Earth today, "Roof of the World." Formation history of the Tibetan Plateau can be divided into nine stages of development (1) Sinian period: Qinghai-Tibet Plateau is divided into two main Gugangwana mainland and Qilian, Gugangwana the mainland in the west, which is now the Himalayas, mountains and Tanggula Gangdise pulse area, located in Qinghai-Tibet Plateau Qilian Eastern, which is now along the Kunlun Mountains and the Qilian Mountains; (2) Cambrian to the Ordovician Period: Gugangwana continent sinking, Qilian its expansion, the scope of the original Tethys significant contraction; (3) Ordovician to the Silurian period: Gugangwana the mainland and further down, Qilian gradually disappear, the original location of Qilian uplift; (4) Devonian to Permian: There Gondwana and the Tethys Ocean and the Eurasian continent, the central plateau once again sink to the ocean; (5) Permian to the Triassic: the original area of central and eastern Qilian rise again to the mainland, the west sinking to deep water and shallow Gondwana and its connected; (6) Jurassic: the Tethys Sea has been uplifting for the land, ocean to the western and northern expansion, the formation of Neo-Tethys; (7) Jurassic to the Cretaceous: the Neo-Tethys contraction Laguigangri first uplift, the formation of a small area south of the sea; (8) Cretaceous to Early Tertiary: the Neo-Tethys closed all, the basic shape of Eurasia; (9) Third Millennium: the collision of the Eurasian plate heated to promote large-scale volcanic and seismic activity, so that the uplift of the Tibetan Plateau increased dramatically. Qinghai-Tibet Plateau over 4000 meters above sea level on average, the highest plateau in the world. The edge of the Himalayas, 8848 meters, is the world's highest mountain. Qinghai-Tibet Plateau and the Himalayas, but the beginning is not so tall, according to geologists research, along the Qinghai-Tibet Plateau and the Himalayas was originally a sea, then lifted it into a collision of continental plates look like today, and the highest plateau in this and mountains in the geological history of the era is still in infancy, will continue to increase. The formation of the Loess Plateau Indian plate moving northward with the Eurasian plate collision, the Indian continental crust into the earth's crust under the Asian continent, and the latter backwater up. Shallow sea which disappeared in the Himalayas, the Himalayas began to form and gradually rose gradually, Qinghai-Tibet Plateau is also the compression uplift of the Indian plate up. This process lasted more than 6000 years later, to about 240 million years ago, more than 2,000 meters of the Qinghai-Tibet Plateau. Tremendous changes in the surface morphology directly change the atmospheric circulation pattern. Prior to this, the Chinese mainland east of the Pacific, north of Siberia and the Himalayan region of south were dominated by shallow seas, the Mediterranean in the west stretching from Central Asia at that time far, so most of the flat in mainland China can be adequately Ocean warm air moisture, warm and humid. Most of northwestern China and Central Asia subtropical inland regions, there has been no large-scale desert and Gobi. Inland in northwestern China and Central Asia and the Gobi desert, because of the drastic changes of hot and cold temperatures, where the crack rock collapse more quickly than elsewhere, as debris, a geologist at the order of the diameter and divide them into: gravel (greater than 2 mm), sand (2-0.05 mm), silt (0.05-0.005 mm), clay (less than 0.005 mm.) Clay and silt particles, can be taken to an altitude of over 3,500 meters into the westerlies, the westerly jet stream is moving southeast, along the Yellow River until gradually falling down. There are hundreds of ancient China at about the "rain dust", "Rain loess," "Rain sand," "Rain haze," the record, the first "rain dust" records date back to 1150 BC: Four Sky Huang Wu plug, sand fell from the sky like rain. This record is actually a dust storm. The location of rain, mainly in the Loess Plateau Soil and near. The ancients such things as disaster strange phenomenon, I believe this is the "Heaven and Man" as a sign. Jin Zhang naturalists prepared to write a blog: "Xia Jie, when, for the night among the palace in the valley, men and women and domestic, no hearings ten ten days, the day is wind blowing, overnight fill in this lonely valley." 1966-1999 years, in our continuing more than two days of dust storms as high as 60 times. CAS Academician Liu Dongsheng, Loess Plateau should be said that a laboratory dust storms, the lab has been the accumulation of dust storms over the past millions of years of records. And the Gobi Desert in northwest China sky diffuse to sprinkle the sand over, every year in the Loess Plateau, leaving a thin layer of loess.
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The development of the plateau
The development of the Loess Plateau Loess Plateau and the Yellow River region was the main arena of the ancestors of the Chinese nation is the birthplace of ancient Chinese culture, has been called the cradle of the Chinese nation. Ancient Xia, Zhou, Qin culture is nurtured to grow here. Today's Loess Plateau, including Shaanxi, Gansu, Ningxia, Shanxi, Henan, Qinghai and Inner Mongolia, seven provinces and autonomous regions, most or part of 200 counties, with a total area of approximately 59.9 million square kilometers, 1.8 million mu of cultivated land area, population nearly 7,000 million. In this vast region, where about 43 million square kilometers of soil erosion, soil erosion per square kilometer per year the amount, by the thousands of tons to 1 million tons. According to the survey estimated that each year 0.5 cm away from the surface erosion of fertile soil. The region of about 2 million mu of cultivated land, as the result of long-term soil erosion, the natural environment, production conditions have been seriously damaged, backward agricultural production in some areas, only 30 to 50 mu kg of grain. July 1977, a more than 150 mm of rain led to flooding from the nearby highlands unimpeded straight down the drain, has submerged more than half of Yan'an City. It is estimated that the annual average erosion modulus of the Loess Plateau (an annual loss in the unit area of sediment volume) is generally 5000 to 15,000 tons per square kilometer, the northern part of Shaanxi and Shanxi in northern and even some places as high as 15,000 to 30,000 tons per square kilometer. Sada mud into the river each year 1.6 billion tons or more. The Loess Plateau, soil erosion, not only seriously jeopardize agricultural production in the Northwest region, but also a serious threat to the safety of the Yellow River, the riverbed of the Yellow River silt constantly high, rare in the world, "hanging river" At present, Lower Yellow River has been 3 to 8 meters above the ground in some places as high as 12 meters higher than the long walls of Kaifeng, a serious threat to downstream lives and property safety. Loess Plateau in the terrain can be divided into three parts. (1) west of central Gansu Liupanshan plateau about 2,000 meters above sea level. There are a number of narrow highland valley plains, such as the Yellow River valley near Lanzhou, Tao River valley near Lintao, are the most affluent places in the highlands. When we walk in the Loess Plateau, you'll see that Mak millet in the field below oily, with neat rows of caves, and that is part of the Loess Plateau on the homes of farmers. (3) in the Taihang Mountains in Shanxi plateau between and Luliangshan. High because there are many faults in Shanxi and local basin, Shaanxi and Gansu highland terrain than the more complex. Steep east slope of the Taihang Mountains, west gentle slope, in fact constitutes a part of Shanxi Plateau. The eastern edge of the Shanxi plateau above 2000 meters above sea level, west gradually reduced, so more than the plateau surface elevation ~ 2000 meters in 1500. The plateau is about 1,000 meters above sea level there are many local basins, such as Binh Dinh, Qinxian County, Changzhi and other basins. Luliangshan similar to the shape of the Taihang Mountains, the highest mountain at 2500 meters above sea level, east slope of the mountain is steep Wei, West Pohuan oblique, becoming connected with the Northern Plateau. Between Luliangshan and between the central Shanxi Taihang there is a narrow lowland, 400 ~ 800 meters above sea level, from the southwest of Taiyuan, Shanxi Yellow River has been extended to the bank. Taiyuan, the ground near one of the widest range, about 150 km, 50 km wide, constitute the largest part in Shanxi Plateau basin. Low-lying roughly parallel to the trend of the Taihang Mountains and Luliangshan, and follow the lowlands into the Fen River, so this low as Fen lowlands. Often low due to a significant fault on both sides, so from a geological point of view, it is a typical Fen lowland grabens. After the founding of new China, the state of governance and development of the Loess Plateau, although a lot of work to do, but because of the production aspects of policy and governance measures, there are some problems, so slow to change the face of the Loess Plateau. Summary of national authorities in the past on the basis of lessons learned, has been initially proposed for future construction in the Northwest Loess Plateau, the approach to be taken. Accounted for a large area of the Loess Plateau, the most serious soil erosion and hilly areas, forestry, animal husbandry should be based, comprehensive development of agriculture, forestry, animal husbandry, according to local conditions, comprehensive management; and according to different natural conditions and socio-economic conditions, the Loess Plateau divided into four different types of areas: (1) agricultural area, including the Weibei, Gansu, Jinzhong, and other places south of Yan'an City. Here are moderate and cold temperature semi-humid climate, annual precipitation of 500 to 600 mm, annual average temperature above 10 ℃, Plateau more production potential. These areas should be the main development of agriculture, food Zijiyouyu do, some counties should be built of commodity grain, cotton and oil base. Tianlin to actively create a protection, slope forest, hill slope at the source surface and proper pasture areas, the development of livestock industry. (2) forest and pastoral areas, including the Longnan, Ningxia, northwestern Shanxi, north of Yan'an City, hilly areas and other regions. Here are the forest-steppe and steppe zones of transition, semi-dry and cold temperature climate, annual precipitation of 400 ~ 500 mm, soil erosion is very serious; the east and the critical wind area, wind erosion has been threatened; cultivated a very large area, the vegetation being serious damage; agriculture by the terrain and climate, and production is low and unstable. This area should be planting trees and grass, the development of forestry and animal husbandry, mainly in "rivers" and the gentle slope on the right platform to build basic farmland, the case for food self-sufficiency in the year. (3) pastoral areas, including Gansu, Ningxia, Shanxi northwest, north of Yulin, some parts of the northern Inner Mongolia. Here are the steppe zone and the desert steppe zone, semi-dry and cold climate, the majority of annual precipitation of 400 mm below the long, cold winter, dry spring and summer and more windy, sandy soil is great, very severe wind and water erosion, crop growth period short, the development of more adverse conditions in agriculture. Development of animal husbandry in this area should be mainly vigorously to create windbreaks, forest grazing, appropriate development of agriculture, food self-sufficiency for. (4) forest, including Ziwuling, Huanglong Hill, Laoshan, Joe Mountain, Mountains, Long Hill neighborhood and parts of counties as part of Luliang mountain areas where. This heavy rainfall, higher ground, most of earth and rock hills, thin soil, and now a number of secondary forest remnants. This area should be based on forest-based, strict protection of existing forest areas, to actively develop this area of water conservation forests in order to protect the development of agriculture and animal husbandry. In short, the plateau of the main crop is barley, which is a kind of barley; unique livestock are yak, together with the Tibetan goats, Tibet is the Qinghai-Tibet alpine pastoral sheep, the three main livestock. Huangtugaoyuan different regions should be based on natural conditions, socio-economic situation and the need for modernization of agriculture, forestry, animal husbandry were developed zoning and implementation of the development of production planning, to the soil and water conservation as the center, improving soil and water management Jie He, slope and Treatment groove binding, combining engineering measures with biological measures, and actively building basic farmland, great forests and pastures, the small watershed as a unit, centralized management and continuous control, so that will be able to speed up the comprehensive management of the Loess Plateau and reasonable development.
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Chinese Academy of Teachers (1976 -)
Female, born in 1976, PhD in Linguistics and Applied Linguistics. Current employer and the Ministry of Foreign Language, Graduate School of Chinese Academy of Sciences Educational background (university onwards) 1994-1998 Harbin Institute of Technology Undergraduate Master of Harbin Institute of Technology 1998-2000 Dr Beijing Foreign Studies University 2000-2003 Work experience, Graduate School of Chinese Academy of Sciences since 2003 --- Foreign Language Department teachers
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Second Shaanxi TV director (1935 -)
Born in March 1935, Shaanxi Chang'an, graduated from Normal School Chang'an, Shaanxi, radio and television speech in group work as band leader. Nearly two decades of television art career, shot a total of "Magpie Tears", "recovery of the youth", "Garden Street, V", "early summer", "black jade river", "Qin Yun", "Ripples Love" "Crazy fleet," "pure rivers" and other odd TV _set_s. The "Magpie Tears" won the 1983 the first public television, "Golden Eagle Award", the first development in Shaanxi Province Award: "Garden Street Five" Award by the Northwest Review of him. Now the China Television Artists Association, Zhongguoshixie Shaanxi Branch of Deputy Secretary-General of the Chinese Musicians Association, Shaanxi Branch. (
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Revolutionary martyr (1904-1961)
Plateau (in September 1904 -1961), originally named High King Xuan, formerly known as the East High look, Old and Zhao Yumin, etc., Shandong Wu Ho Liu Zhuncun County (now part of Hebei Gucheng) people. Communist Party members. 7-year-old into the private school, 11 years on the county senior primary, 14-year-old admitted to the private Zhengyi school of Jinan, Shandong Provincial age of 16 into the third Teachers (located in Liaocheng), 21-year-old admitted to the Beijing Private Chinese University. High school, by the "May Fourth" Movement of Patriotic Movement and the New Culture, accepted the thinking of many of the democratic revolution. 1925, "Divergence" tragedy, the struggle in Beijing participated in the strike, and actively supported the British General Feng Yuxiang, Japan declared war on ideas. To fight in the national crisis, Toubicongrong, was admitted to Northwestern Army in 1926 Cadre School. In school, with the Communists had contact, and a lot of communist propaganda theory of reading books. May 1926, high by the students according to Yu, Zhang Yuchen introduction, joined the Chinese Communist Party. In the same year in October, sent by the party, went to the Soviet Union with the Northwest Army tours to visit the officers of the regiment is responsible for state of mind to grasp, to the representatives of our party to the International Tan Pingshan report. April 1927, Chiang Kai-shek betrayed the revolution, tour the same year between June to July back to Luoyang. Kaifeng, Henan Provincial Party Committee found him to, any party branch secretary of the streets in Kaifeng, and participated in the South Han Chen gay editor of the "inspection tour Russian mind," a book editing and proofreading. February 1928, Special Committee of CPC northern Anhui, Ministers of the Organization, and is also the Communist military correspondent in Yang and Northwest Military. In the same year early April, in Fu Yang, flow _set_ to launch the uprising. Back home, and actively promote communist ideology, circulated progress books. January 1930 to 9 months, Kaifeng served as anti-imperialist Anti-Imperialist League and Youth League caucus, the military correspondent of Henan provincial party committee in Kaifeng, Kaifeng soldiers riot commissions, Henan Province, Central Military Commission, Chief of Staff and other staff. In the same year in September, was arrested by riot soldiers planning. April 1931, by Liu Peixia, South Han Chen (when he was Secretary-General of the Henan Provincial Government) and other comrades to rescue from prison. Later in Tianjin, Jinan, in the party's intelligence. The end of 1934, to Shanghai to do the party's intelligence. War broke out in 1937 to "armed anti-Japanese East China will be the" responsible person on behalf of, the development of some anti-Japanese organizations and intelligence organizations for the development of anti-Japanese armed revolutionary forces grow and make a positive contribution. January 1940, he served as Director in Southern New Fourth Army Judge Advocate Division, branch secretary. In 1945, he served in Northern Area Committee of the regional party committee deputy secretary of the enemy and the enemy and Industry Deputy Minister of the regional party committee. After October the same year, served as the Northeast Bureau of the CPC Central Committee, Deputy Director of Social Intelligence, provincial Information Minister Liaodong Liaodong Branch Information Commissioner and other staff. 1950 to 1956, served as the first Director of East China Military and Political Committee, East teacher training cadres, Ministry of Justice, Ministry of Justice, Office of the East, Supreme People's Court East Branch, East China, director of the Ministry of Justice and Judicial Reform under one roof with the Office of Director, East China Commission Deputy Secretary-General of Shandong Provincial People's Committee Office of the Deputy Director of Law and Shandong Provincial People's Committee Deputy Secretary General and other staff. September 1961, died in Jinan.
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China researcher at the Institute of Earthquake Prediction
Male, born in 1964, Ph.D. Geophysics (1999, University of Science and Technology of China), China researcher at the Institute of Earthquake Prediction, PhD supervisor (Institute of Geophysics, China Seismological Bureau.) 1998-1999 Institute of Technology in Zurich, Switzerland to study (ETH) ,2002-2003, he went to Edinburgh University to do postdoctoral research. Made in Japan Visiting Professor, University of Tokyo (2000), 2003-several times in 2005, a visiting professor at the University of Edinburgh, to carry out collaborative research, is responsible for an earthquake in the British science and technology cooperation projects with the National Natural Science Foundation and The Royal Society joint funding. Currently engaged in seismic anisotropy, crust and mantle structure, digital seismic data in the strong short-term prediction of earthquakes and crustal stress analysis and other research. • in the domestic part of the research papers published in journals: Plateau, Teng JW, 2005. China's continental crust and upper mantle seismic anisotropy. Progress in Geophysics, 20 (1): 180-185. Plateau, Liang D, cloves, Xue Yan, Cai Mingjun MATHEMATICS AND Su Jin, Peng Liguo, 2004. Earthquake in Yunnan Province in 2001 Shidian shear-wave splitting parameter variation. Seismological Journal, 26 (6): 576-582. English: Gao, Y., Liang, W., Ding, X., Xue, Y., Cai, M., Liu, X., Su, Y. & Peng, L., 2004. Changes in characteristics of shear- wave splitting of earthquakes in Shidian, Yunnan, China. ACTA Seism. Sinica, 17 (6): 635-641. Plateau, MATHEMATICS AND Leung D, Hao Ping, 2004. Shear-wave splitting system analysis method (SAM) software system. China Earthquake, 20 (1): 101-107. English: Gao Yuan, Liu Xiqiang, Liang Wei and Hao Ping, 2004. Systematic analysis method of shear-wave splitting: SAM software system, Earthquake Research in China, 18 (4): 365-372. Plateau, Suzan van der Lee, Domenico Giardini, Jochen Braunmiller, Si-Hua Zheng, 2001. Using the mode superposition method of 8 November 1997 Mani earthquake focal mechanism of Tibet. Geophysics, 44 (Suppl.): 98-106. Plateau, 2000. Critical state of rupture marble shear wave splitting. China Earthquake, 16 (3): 197-202. Plateau, Hui-Lan Zhou, Ma Yan Road, 2000. Touch base in Sichuan-Yunnan region of seismic activity. China Earthquake, 16 (1): 86-91. English: Gao Yuan, Zhou Huilan and Ma Yanlu, 2000. SLC analysis on earthquake activity in the regions of Sichuan and Yunnan of China Earthquake Research in China, 14 (3): 277-283. Plateau, Shi-Yu, Hui-Lan Zhou, Xiaohong, Liu Qiliang, 1999. Shear-wave splitting marble differential stress response of experimental study. Geophysics, 42 (6): 778-784. [09] Plateau, Si-Hua Zheng, Hui-Lan Zhou, 1999. Polarization of fast shear wave in Tangshan region and changes the image. Geophysics, 42 (2): 228-232. [08] Plateau, Si-Hua Zheng, Hui-Lan Zhou, Liu, Wu ZL, 1997. A complex earthquake rupture characteristics. Seismological Journal, 19 (1) :1-6 English: Gao Yuan, Zheng Si-hua, Zhou Hui-lan, Liu Zhen and Wu Zhong-liang, 1997. Analysis on rupture feature of a great complicated earthquake in Kamchatka. ACTA Seismologica Sinica, 10 (1): 1-6 [07] Plateau, Si-Hua Zheng, Wang Peide, 1996. Hainan Province in the eastern areas in 1992 small earthquake swarm of shear wave splitting. Geophysics, 39 (2) :221-232. [06] Plateau, Wu ZL, on November 13 1995.1993 Kamchatka earthquake rupture process and tectonic implications. Geophysics, 38 (1) :55-63. English: Gao Yuan and Wu Zhong-liang, 1995. Rupture process of the 13 November 1993, Kamchatka, Ms7.1 earthquake from broadband waveform analysis and its tectonic implications. Chinese Journal of Geophysics, 38 (1): 79-88. [05] Plateau, Liu Zhaojun, 1995. Stochastic cellular automata simulation of the dynamics of seismic implications. China Earthquake, 11 (1) :8-13. English: Gao Yuan and Liu Zhao-jun, 1995. Dynamical implications of earthquake modeling using stochastic cellular automata. Earthquake Research in China, 9 (4): 379-385. [04] Plateau, Wu ZL, 1995. Broadband teleseismic body waves with a record of 2 October 1993 6.2 earthquake in southern Xinjiang, China source process. China Earthquake, 11 (2) :147-160. [03] Plateau, Si-Hua Zheng, Sun Yong, 1995. Tangshan crust fracture anisotropy. Seismological Journal, 17 (3) :283-293. English: Gao Yuan, Zheng Si-hua and Sun Yong, 1995. Crack-induced anisotropy in the crust from shear wave splitting observed in Tangshan region, North China. ACTA Seismologica Sinica, 8 (3): 351-363. [02] Plateau, Si-Hua Zheng, 1994. Shear wave splitting in Tangshan region (Ⅱ) - correlation function analysis, the Chinese earthquake. 10 (Suppl) :11-21. English: Gao Yuan and Zheng Si-hua, 1995. Cross correlation function analysis of Shear wave splitting - method and example of its application. Journal of Earthquake Prediction Research, 4 (2): 224-237. [01] Si-Hua Zheng, Plateau, 1994. China lithosphere anisotropy. Seismological Journal, 15 (2) :131-140. English: Zheng Si-hua and Gao Yuan, 1994. Azimuthal anisotropy in lithosphere on the Chinese mainland from observationa of SKS at CDSN. ACTA Seismologica Sinica, 7 (2): 177-186. • published in foreign journals part of the research paper: Gao, Y., Hao, P. & Crampin, S., 2006. SWAS: A shear-wave analysis system for semi-automatic measurement of seismic shear-wave splitting above small earthquakes. Phys. Earth Planet. Inter., 159 ( 1 / 2): 71-89. doi: 10.1016/j.pepi.2006.06.003 Wu, J., Crampin, S., Gao, Y., Volti, T. and Chen, Y.-T., 2006. Smaller source earthquakes and improved measuring techniques allow the largest earthquakes in Iceland to be stress-forecast (with hindsight). Geophys. J. Int., 166 (2): 1293-1298. doi: 10.1111/j.1365-246X.2006.03054.x [09] Crampin, S. and Gao, Y., 2005. Comment on "Systematic Analysis of Shear-Wave Splitting in the Aftershock Zone of the 1999 Chi-Chi, Taiwan, Earthquake: Shallow Crustal Anisotropy and Lack of Precursory Changes, by Yungfeng Liu, Ta-Liang Teng, and Yehuda Ben-Zion ". Bull. Seism. Soc. Am., 95 (1): 354-360 [08] Gao, Y. and Crampin, S., 2004. Observations of stress relaxation before earthquakes. Geophys. J. Int., 157 (2): 578-582. [07] Crampin, S., Peacock, S., Gao, Y. and Chastin, S., 2004. The scatter of time-delays in shear-wave splitting above small earthquakes. Geophys. J. Int., 156 (1 ): 39-44. [06] Gao, Y. and Crampin, S., 2003. Temporal variations of shear-wave splitting in field and laboratory in China. J. Appl. Geophys .. 54: 279-287. [05] Crampin, S., Chastin, S. and Gao, Y., 2003. Shear-wave splitting in a critical crust: III - preliminary report of multi-variable measurements in active tectonics. J. Appl. Geophys., 54 : 265-277. [04] Crampin, S., Gao, Y., Chastin, S., Peacock, S. and Jackson, P., 2003. Speculations on Earthquake Forecasting. Seism. Res. Lett., 74 (3) :271-273 [03] Gao, Y., Wu, Z.-L., Liu, Z. and Zhou, H.-L., 2000. Seismic source characteristics of nine strong earthquakes from 1988 to 1990 and earthquake activity since 1970 in the Sichuan -Qinghai-Xizang (Tibet) zone of China. Pure Appl. Geophys., 157 (9): 1423-1443. [02] Gao, Y., Wang, P.-D., Zheng, S.-H., Wang, M., Chen, Y.-T. and Zhou, H.-L., 1998. Temporal changes in shear-wave splitting at an isolated swarm of small earthquakes in 1992 near Dongfang, Hainan Island, southern China. Geophys. J. Int., 135 (1), 102-112. [01] Wu, Z.-L. and Gao, Y., 1994. Scaling law of earthquake energy: a modification in the view of broad frequency band. Fractals, 2 (4): 583-588.
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The late Secretary for the Ministry of Communications Science and Technology
Former Highland High Bao Qi, Hebei Yongqing people born in May 1915, in February 1936 as head of the Tsinghua University student, in the secret struggle against the Japanese. September 1938 joined the Communist Party of China. October 1937 the General Command of the Eighth Route Army Division One, Second Division, he served as military director of the Department of Hongliugou Iron Works. August 1945 served as defense minister from the government building factories Chief Engineer, Highway Administrative Office of the Secretary of Taihang, North China, Traffic Engineering Director, was responsible for the construction of the road was the largest suspension bridge Zhuozhang. October 1949 from the Former Central Administration of the Ministry of Communications Deputy Director Flight Operations Engineering, water Design Institute, Technical Secretary. January 1959 transferred the work of Chinese Academy of Sciences, has Ren Changchun, director of precision machinery, new technology department in the number of such posts, deputy director of the Faculty of Physics and Chemistry. April 1973 the Ministry of Communications Science and Technology Commission of any charge. November 1979 appointed Secretary of Science and Technology Ministry of Communications, Science and Technology Secretary and Transport Academy of Sciences. Retired in December 1982. Vice-ministerial level, the ministerial medical treatment. April 30, 2007 in Beijing, died at 92 years old. Plateau, female, graduate student in 1988 graduated from Northwest Normal University, a master degree. Lanzhou City College is currently a professor of Chinese literature, Associate Director. In ancient Chinese literature, ancient Chinese thought and culture and aesthetics teaching and research of traditional Chinese culture holds a deep warmth and respect, dedicated to cultural heritage of modern classic. Representative papers are: "The Book of Songs】 【comprehensive theory of errors", "" seclusion, "the new concept of Tao is also implicit non-hidden", "Guo Xiang" Happy feet of the "theory" and "pain into beauty into despair Sublimation - the happy ending of life of Tao "," "Pan Peasant Consciousness," mantra - and Western socio-cultural Perspective to the theme】 【Water Margin "," novel quatrains - On the poetic novel, "said New World language "," "extremely moderate Realm Road - On the Tao <mao-year-old lands and the beginning of spring nostalgia> two", "China's first poetry - poems Tao】 【alcohol (Fifth) Value of On, "" the doctrine of Tao. " Monograph: "I aesthetic I exist", "Tao Yuan Dynasty - extremely sophisticated road moderate." Professor Gao Yuanfu, female, March 1962 Health, Shandong Anqiu who graduated in 1983, Department of Chemistry, Xuzhou Normal University, stayed on to teach after graduation in 1997, transferred to Teachers College, Shenzhen University, Department of chemical and biological weapons. For a long time, mainly in organic chemistry, inorganic chemistry, teaching and fine organic synthesis, organic synthesis, new methods of research. _Set_ off for the undergraduates, "Organic Chemistry", "Organic Synthesis", "Advanced Organic Chemistry", "Organic Chemistry", "Inorganic Chemistry", "Structure and Properties", "basic immunology and pathogen biology," and so on. Chaired the Education Commission, Jiangsu Province, undertaken over a number of research projects and schools to participate in a National Natural Science Foundation of commitment. In the solid-phase organic reactions, new methodologies for organic synthesis and other fields have made a lot of fruitful work, the results in the "Syn.communication", "Organic Chemistry", "CJof Chemistry", "Tetrahedron Letters", "Structural Chemistry" , "Chinese Chemical Letters", "Chemical Technology", "Applied Chemistry", "chemical reagents", "Pharmaceuticals" and other publications published dozens of research results in academic circles at home and abroad have a greater impact more than 20 papers have been SCI. Papers published in 2001 which has eight were SCI, there are nine in 2002 was SCI.
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Encyclopedia
Plateau plateau gaoyuan Plateau (nl ateau) edge of steep slopes, the top level Slow wide, 500 meters above sea level over the general area. To The larger the absolute height or relative height different from the plain, The broad flat top surface different from the mountains. Plateau to special Some of the terrain topography and high-pitched as the natural environment Important factor in the formation and development, the formation of a special high altitude air Climate, hydrological conditions and biological type of military action is Different from the mountains and plains of the special operations environment. Most of the crust after a long plateau is a large range of continuous Wai-shaped lifting surface (ie, uplift of continental plates), or primitive Surface as lava, sediment formed by the coating. The Canyon Ditch Sink partition, often become long and narrow flat-top height roughly equal Ridge, is the difficult access, large-scale military operation is not easy The area. Plateau at the top surface morphology can be divided into four kinds: ① Ping Tanzania plateau, the top wide, nearly flat. Such as the Mongolian high The original, bare rock surface is mainly shallow depressions and ridges Kong. ② units like the plateau, the top surface by a combination of multi-platform Cheng, Chang Cheng-order-like shape. Such as the Central Siberian Plateau, in the Angara River and the lower Tunguska River valley in 9-14 Terrace. ③ hummocky plateau, wavy or appear before the top of hills Distribution. Such as the Deccan Plateau of the Indian subcontinent (see India), the Department of erosion by the river cutting, and more residual hill, horst and sewer. ④ Gangluan rolling plateau, the top surface of a hill valley basin distribution, from V obvious. Such as the South African plateau, the region from the wide-shallow basin Alternating with the table-like platform. The different plateau Level the top and cut into different military action Affected areas. According to the location of the plateau can be divided into 3 Categories: ① mountain plateau between the community in the mountains, often with the mountains At the same time to form, part or all surrounded by mountains. Such as China Qinghai-Tibet Plateau, is a series of things that lie in the tall Mountain ranges of the mountains of the plateau, the terrain is very high, the top wide Wide, thin air, changing weather, cold weather, topography Barrier, transport facilities, the military has a natural barrier for Use, is also a serious impact on military operations for the special Warfare environment. Peninsula of Asia Minor Anatolia plateau, South, North, East, surrounded on three sides by mountains, is a mountain Plateau. ② Piedmont Plateau, located in the mountain side, the other side With plain or marine phase, mostly ribbon extension. Such as South America Patagonia Island, west of the Andes, East Adjacent Atlantic Ocean, lying east tilt, ladder-shaped, coastal Gaoya hanging around steep, with only a narrow coastal plain, which will help Haiphong. ③ continental plateau, located in the continental interior, wider than Large continental plateau and adjacent plains or sea around the Ariake Significant height difference. Deccan Plateau to the Indian subcontinent such as India's main Body, and the western edge of Western Ghats, a steep slope, the East Edge of the Eastern Ghats, gentle slope, a narrow coastal Plain. Plateau mainly located in the middle of the continent. World's largest The plateau is the plateau of Brazil in South America (see Brazil), surface Of approximately 500 million square kilometers; the highest plateau of China Qinghai-Tibet Plateau, with an average altitude of 4000 meters. China Plateau area of about 2.5 million square kilometers, there are known the world Ridge of the Qinghai-Tibet Plateau sector, micro-relief undulating high in Inner Mongolia Original, multi-mountain valleys of the Yunnan-Guizhou Plateau and gullies Ordos Plateau. Plateau on the Army