| 黔南桂西中三叠统浊积扇、物源及板块构造 |
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| 引用本文： | 秦建华,吴应林.黔南桂西中三叠统浊积扇、物源及板块构造[J].沉积与特提斯地质,1989,9(3):1-17. |
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| 作者姓名： | 秦建华 吴应林 |
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| 作者单位： | 成都地质矿产研究所，成都地质矿产研究所 |
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| 摘 要： | 引言广布于黔南桂西地区的中三叠世重力流沉积物(面积达7000km~2),由于在黔桂盆地的沉积演化历程中,占有重要地位,因而,历来为世人所注目。近年来,国内先后有许多单位和个人(西南石油学院地质系,1978、1979;张继淹,1985;苟汉成,1985;贺自爱,1956;)曾就这套沉积物形成的地质背景,沉积机理进行过有益的论述。但迄今为止,尚意见纷纭,争论颇
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Middle Triassic Turbidite Fan,Source Area and Plate Tectonics in Southern Guizhou and western Guangxi |
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| Qin Jianhu,Wu Yinglin.Middle Triassic Turbidite Fan,Source Area and Plate Tectonics in Southern Guizhou and western Guangxi[J].Sedimentary Geology and Tethyan Geology,1989,9(3):1-17. |
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| Authors: | Qin Jianhu Wu Yinglin |
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| Institution: | Chengdu Institute of Geology and Mineral Resources |
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| Abstract: | Caused by tectonism, the Middle Triassic gravity flow deposits covering an area of 7000 square kilometres are widely distributed over southern Guizhou and western Guangxi. According to their origins. mudstone and conglomerate resulted from debris flow and turbidite from turbidity current may be distinguished. The turbidite fan model. the main sedimentary model, is characterized by multiple stages and progradation of the turbidite fan which trends to be elongated during the early stage of formation and radial during the later stage. varying with the features of the deposits. The results from sedimentary facies, palaeocurrent direction, petrology, geochemistry and mathematical geology show that the sedimentary system of gravity flow is developed in the marginal back-arc basins, and evolved due to tectonism from turbidite fan(Bannaian)through slope aprons(later Bannaian) to the mixed system of turbidite fan and slope aprons(Lanmuian). The North Vietnam oldland situated in the southwestern part of the turbidite basin is believed to be the main source area for the gravity flow system. |
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