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《Geotectonica Et Metallogenia》 2006-03
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STATIC FRAMEWORK AND DYNAMIC EVOLUTION OF WESTERN TAIWAN FORELAND BASIN

WANG Hairong 1,2, WANG Yingmin1, LIU Zhenhu3, ZHOU Aihua 1,2 and HUANG Qizhi4 (1. MOE Key Laboratory for Hydrocarbon Accumulation Mechanism Study, University of Petroleum, Beijing 102249, China; 2. Basin and Reservoir Research Center, University of Petroleum, Beijing 102249, China; 3. Institute of Guangzhou Marine Geological Survey, Guangzhou, GD 510760, China; 4. China Petroleum & Gas Exploration and Development Corp., Beijing 100083, China)  
Based on research about the trench-arc-basin system, its geodynamic mechanism, tectonic units like orogens and forelands, a 4-stage model about the evolution of Western Taiwan Foreland Basin was proposed in this paper. The model consists four stages, namely, 1. Stage of accretionary wedge development - unidirection source. Although the developing accretionary wedge was superimposed on the passive continent strata (PCS) during this phase, the profile of basin still retains characteristics of classical PCS and the continent remains as the only source of material for depositing. 2. Stage of response of flexing - bidirection source. During this phase response of flexing is becoming more and more evident, accretionary wedge begins to play an increasingly important role of supplying material to basin, but the continent is still the major source of material for deposition in the basin. 3. Stage of formation of foreland system. During this phase foredeep, especially forebulge, was formed. The spectacular orogen in the hinterland becomes the major source of depositing materials. The classical foreland depositional wedge is formed and overlaps towards the forebulge gradually. 4. Stage of collapsing of orogen - waning of foreland. During this phase extension commences and expands rapidly. Denudation happens to those foreland strata owing to the uplifting of foredeep and volcanism appears again impressively. Eventually, discussions were made about a detailed explanation on hard-to-be-unraveled questions available and some further thoughts were proposed.
【Fund】: 国家重点基础研究发展规划项目(G200004670502).
【CateGory Index】: P542.2
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9 CUI Xuejun 1, XIA Bin 1, ZHANG Y H 2, LIU Baoming 1 , WANG Ran 1 and YAN Yi 1 (1. CAS Key Laboratory of Marginal Sea Geology and Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. CSIRO Exploration & Mining, P.O.Box 1130, Bentley, WA 6102, Australia);A NUMERICAL MODELING STUDY ON THE “ASTHENOSPHERE UPWELLING” OF SOUTH CHINA SEA[J];Geotectonica Et Metallogenia;2005-03
10 Zhu Bingquan Wang Huifen(Institute of Geochemistry, Academia Sinica);Nd-Sr-Pb ISOTOPIC AND CHEMICAL EVIDENCE FOR THE VOLCANISM WITH MORB-OIB SOURCE CHARACTERISTICS IN THE LEIQIONG AREA, CHINA[J];Geochimica;1989-03
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