QUANTITATIVE SUBSIDENCE ANALYSIS OFTHE TENSIVE BASIN AND COMPRESSIVEMOUNTAIN TYPE DIWA BASIN WITH IMPLICATIONS FOR EPISODIC TECTONIC MOVEMENT AND SEDIMENTATION
QUANTITATIVE SUBSIDENCE ANALYSIS OF THE TENSIVE BASIN AND COMPRESSIVE MOUNTAIN TYPE DIWA BASIN WITH IMPLICATIONS FOR EPISODIC TECTONIC MOVEMENT AND SEDIMENTATION
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1DIWA STRUCTURES IN THE WORLD[J].Geotectonica et Metallogenia,1999,23(2):173-184.
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2G. Andreev(Buryat Geological Institute, Ulan-Ude, Str. Sahyanova 6, 670042, Russia).PECULIARITIES OF METALLOGENY OF SOUTH SIBERIA AND WEST MONGOLIA DIWA REGIONS[J].Geotectonica et Metallogenia,1995,19(1):22-26.
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3L. V. Grigorieva and N. F. Shinlarev(St. Petersburg State University , Russia).GEOLOGY AND METALLOGENY OF PRECAMBRIAN ACTIVIZATION (PROTODIWA) IN CONCERN OF PRECAMBRIAN EARTHCRUST EVOLUTION[J].Geotectonica et Metallogenia,1995,19(4):39-47. 被引量：1
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4DIWA STRUCTURES IN THE WORLD[J].Geotectonica et Metallogenia,1999,23(1):84-96.
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5ZHANG Jinjiang, DING Lin, ZHONG Dalai & ZHOU Yong Institute of Geology and Geophysics. Chinese Academy of Sciences. Beijing 100029, China.Orogen-parallel extension in Himalaya: Is it the indicator of collapse or the product in process of compressive uplift?[J].Chinese Science Bulletin,2000,45(2):114-120. 被引量：16
