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《Geotectonica Et Metallogenia》 2007-01
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MULTIPLE GEOLOGICAL ELEMENTS CONSTRAINT ON THE MESOZOIC TECTONIC EVOLUTION OF SOUTH CHINA: APOCALYPSE OF THE MESOZOIC GEOLOGICAL EVOLUTION IN SOUTHEASTERN HUNAN AND THE HUNAN-GUANGDONG-JIANGXI BORDER AREA

BAI Daoyuan1, HUANG Jianzhong1, LI Jindong2, WANG Xianhui1,MA Tieqiu1, ZHANG Xiaoyang1 and CHEN Bihe1(1. Hunan Institute of Geological Survey, Xiangtan, Hunan 411100, China; 2. Hunan Bureau of Geology, Mineral Resources, Exploration and Development, Changsha, Hunan 410011, China)  
There are recognizant divergences on the Mesozoic tectonic evolution of south China, which is to a certain extent related to inadequacy of integrated study on multiple geological elements. The authors have recognized that there were different representative geological elements at different Mesozoic tectonic stages in Southeastern Hunan and the border area among Hunan, Guangdong and Jiangxi provinces. The different geological elements suggest different tectonic environment settings. The Early Triassic to the early episode of Middle Triassic is the pre-orogenic stage for occurrence of marine deposits mainly. The late episode of Middle Triassic to the early stage of Middle Jurassic is the intracontinental orogenic stage, which can be further divided into four sub-stages listed as follows: the late episode of Middle Triassic is a peak stage for intracontinental subduction-convergence characterized mainly by a great number of NNE-trending thrusts and folds and NW-trending basement strike-slip faults. A post-collisional tectonic setting exists corresponding to the syn-orogenic stage in the late episode of Middle Triassic-latest Triassic, which is characterized mainly by occurrence of Indosinian highly peraluminous granitoids; A syn-orogenic uplift-extensional tectonic setting occurs in the late episode of Late Triassic-Early Jurassic, which is characterized mainly by down-faulted basins and tholeiite; A compressional tectonic setting occurs in the early episode of Middle Jurassic, which is characterized mainly by occurrence of piedmont thrust-compressional basins and thrusts at basinal margin. The early episode of Middle Jurassic-Late Jurassic is a post-orogenic stage, which is characterized mainly by occurrence of voluminous post-orogenic granite and nonferrous metallic mineral deposits related to granite. The Cretaceous is an intraplate-rifting stage, characterized by representative geological elements such as AA-type granite, red down-faulted basins, bimodal subvolcanic rocks and basic volcanic rocks. Based on these achievements and regional geological study results, the authors hold that the Mesozoic tectonic evolution of South China should be studied in terms of multiple geological elements, and particular attention shall be paid to whether the geological elements for discrimination of structural environment are representative in terms of time limits for geological elements and conjunction of tectonic evolution events.
【Fund】: 中国地质调查局区域地质调查项目(200213000035)资助.
【CateGory Index】: P542
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