Evolution of Circum－Pacific Basins andVolcanic Belts in East China and Their Geodynamic Background

Ｅｖｏｌｕｔｉｏｎ　ｏｆ　Ｃｉｒｃｕｍ－Ｐａｃｉｆｉｃ　Ｂａｓｉｎｓ　ａｎｄＶｏｌｃａｎｉｃ　Ｂｅｌｔｓ　ｉｎ　Ｅａｓｔ　Ｃｈｉｎａ　ａｎｄＴｈｅｉｒ　Ｇｅｏｄｙｎａｍｉｃ　Ｂａｃｋｇｒｏｕｎｄ￥ＬｉＳｉｔｉａｎ（ＦａｃｕｌｔｙｏｆＥａｒｔｈＲｅｓｏ...     

Petrogenesis of Eclogites in the Light of Punctuated Metamorphic Evolution in Dabie Terrane，China

Ｐｅｔｒｏｇｅｎｅｓｉｓ　ｏｆ　Ｅｃｌｏｇｉｔｅｓ　ｉｎ　ｔｈｅ　Ｌｉｇｈｔ　ｏｆ　ＰｕｎｃｔｕａｔｅｄＭｅｔａｍｏｒｐｈｉｃ　Ｅｖｏｌｕｔｉｏｎ　ｉｎ　Ｄａｂｉｅ　Ｔｅｒｒａｎｅ，Ｃｈｉｎａ￥ＹｏｕＺｈｅｎｄｏｎｇ；ＨａｎＹｕｊｉｎｇ；ＺｈｏｎｇＺ...     

Geological Anomaly of China

Ｇｅｏｌｏｇｉｃａｌ　Ａｎｏｍａｌｙ　ｏｆ　Ｃｈｉｎａ￥ＺｈａｏＰｅｎｇｄａ（ＦａｃｕｌｔｙｏｆＥａｒｔｈＲｅｓｏｕｒｃｅｓ，ＣｈｉｎａＵｎｉｖｅｒｓｉｔｙｏｆＧｅｏｓｃｉｅｎｃｅｓ，Ｗｕｈａｎ４３００７４）ＷａｎｇＪｉｎｇｇｕｉ；ＲａｏＭｉｎｇｈｕ...     

Cu－An Metallogenic Series Related to Volcanic－Intrusive Complexes in Eastern China

Ｃｕ－Ａｎ　Ｍｅｔａｌｌｏｇｅｎｉｃ　Ｓｅｒｉｅｓ　Ｒｅｌａｔｅｄ　ｔｏＶｏｌｃａｎｉｃ－Ｉｎｔｒｕｓｉｖｅ　Ｃｏｍｐｌｅｘｅｓ　ｉｎ　Ｅａｓｔｅｒｎ　Ｃｈｉｎａ￥ＺｈａｉＹｕｓｈｅｎｇ（ＤｅｐａｒｔｍｅｎｔｏｆＧｅｏｌｏｇｙａｎｄＭｉｎｅｒａｌＲｅ...     

PALEOMAGNETIC EVIDENCE FOR THE RELATIVE MOTION BETWEEN THE SOUTH CHINA BLOCK AND INDOCHINA BLOCK

The Mesozoic paleomagnetic pole positions from the Indochina block and South China block are not consistent with each other in that the formers are displaced with respect to the latters westward in longitude and southward in latitude. The displacement is here interpreted as to be related to the India-Eurasia collision in such a way that after the collision the Indochina block was rotated clockwise by 8° about the Assam syntaxis, followed by an eastward translation of the South China bl..     

TECTONIC FEATURE OF QINGHAI-XIZANG PLATEAU AND ITS STRESSED STATE

This paper deals with the uplift mechanism and the uplift form of Qinghai-Xizang (Tibet) plateau and the deformation regularity of its surrounding region caused by this uplifting. It is shown that the insertion of Indian plate with the wedge-like frontal margin beneath Qinghai-Xizang plateau made the plateau compressed and uplifted; at same time along several pre-existing large faults, striking NE and NW, the strike-slip movement took place. It is of great significance to study Asian     

COMPILATION OF HEAT FLOW DATA IN THE CHINA CONTINENTAL AREA (2nd Edition

During the last 2 years, heat flow data increased significantly in China as a result of implementation of many comprehensive geodynamic (including geothermal) projects and GGT project in China. In this paper, a total of 366 reliable heat flow data is collected from published and in press sources in the Compi-ilation of Heat Flow Data in the China Continental Area (2nd edition). Statistic analysis of these data shows that the heat flow values in China continental area vary from 20 to 14...     

FLUVIAL PROCESSES IN THE LOWER YELLOW RIVER AFTER LEVEE BREACHING AT TONGWAXIANG IN 1855

I. CHAncEL CHANGal m THE FLOODED AREA ArVER BREACHING AT TONGWAXIANG AND THEIR IMPACTSIn mid--June of 1855 a great flood occurred in the lower reaches of the Yellow River. The findmainly came down from the main stem of the river and itS tributary Qinhe River. In the meantimethe riparian area of the Yellow River had just been subjected to a heavy rain, and large amountS of water from mountains and hills were flowing into the river and lakes were also full. The Weis…     

REE TRACER METHOD FOR STUDIES ON SOIL EROSION

ＲＥＥＴＲＡＣＥＲＭＥＴＨＯＤＦＯＲＳＴＵＤＩＥＳＯＮＳＯＩＬＥＲＯＳＩＯＮＴＩＡＮＪｕｎｌｉａｎｇ；ＺＨＯＵＰｅｉｈｕａａｎｄＬＩＵＰｕｌｉｎｇ（ＴｈｅＥｎｇｌｉｓｈｔｅｘｔｉｓｅｄｉｔｅｄｂｙＭｒｓ．ＳＵＵａｎａｎｄＤｒ．ＤＩＮＧＬｉａｎｚｈｅｎ...     

NUMERICAL SIMULATION OF INUNDATION IN SHENZHEN CITY BY FINTE DIFFERENCE MODEL MIXED WITH 1D AND 2D UNSTEADY FLOW

ＮＵＭＥＲＩＣＡＬＳＩＭＵＬＡＴＩＯＮＯＦＩＮＵＮＤＡＴＩＯＮＩＮＳＨＥＮＺＨＥＮＣＩＴＹＢＹＦＩＮＴＥＤＩＦＦＥＲＥＮＣＥＭＯＤＥＬＭＩＸＥＤＷＩＴＨ１ＤＡＮＤ２ＤＵＮＳＴＥＡＤＹＦＬＯＷ￥ＣＨＥＮＧＸｉａｏｔａｏ；ａｎｄＱＩＵＪｉｎｗｅｉ（Ｓｅｎ...