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《Acta Sedimentologica Sinica》 2008-04
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Discussion on Depositional Characteristics and Basin Quality in Kunlun Orogenic Belt During Early-Middle Devonian

CHEN Shou-jian1 LI Rong-she1 JI Wen-hua1 ZHAO Zhen-ming1WANG Bing-zhang2 MA Hua-dong3 LIU Xiao-ji4 SHI Bing-de1(1.Xi’an Institute of Geology and Mineral Resources, Xi’an 710054;2.Qinghai Institute of Geological Survey, Xining 810012;3.Xinjiang Institute of Geological Survey, Urumqi 830011;4.China University of Geosciences, Beijing 10083)  
The basic tectono-stratum pattern of Kunlun Orogenic Belt, which was the product of ocean-continent transformation and collisional orogeny during Early Paleozoic and Late Paleozoic, was developed on the basis of Paleozoic. The Caledonian collisional orogeny, at the end of Early Paleozoic, made the Early Paleozoic ocean basin close and the whole Kulun area was uplifted to be land. As a sedimentary response to orogeny, the sediments of Early-Middle Devonian foreland basin formed at the piedmont area within the suture zone. The Early-Middle Devonian of East Kunlun mainly distributes in Middle Kunlun and Southern Kunlun. The northern part has sediments formed in the environment of abyssal-bathyal basin, shallow sea shelf and sea-land transition facies while the southern part is littoral-neritic. The sediments are characterised by wedge shape which becomes thinner from north to south in 3-D space. They display characteristics that the environment once changed from abyssal-bathyal to shallow sea shelf finally to sea-land alternation facies in temporal sequence, which reflect that the basin became shallower upward. The material sources were mainly from the northern part, namely the Early Paleozoic Orogenic Belt of Northern Kunlun, the southern part was secondary source area. Because the sediments developed on the subduction landmass, at the end of Silurian when Qimantage ocean basin had closed, they reflect that they have peripheral foreland basin sedimentary characteristics. In West Kunlun, the Middle Devonian only developed in the northern part, while the southwest was mainly abyssal-bathyal basin sediments and the upper developed littoral-neritic sediments, the northern part and the southern margin of Tarim basin developed littoral-neritic sediments. These sediments are wedge-shaped in 3-D space becoming thinner from southwest to northeast. In temporal sequence, their sedimentary environment changed from abyssal-bathyal to shallow sea to sea-land alternation finally to land facies. They also reflect that the basin became shallower upward. The material sources were mainly from southwest orogenic belt, while the Tarim ancient land in the northeast was secondary source area. Considered that the strata developed in the northern part of Middle Kunlun magmatic back-arc, at the end of Ordovician when Kudi ocean basin had closed, it can be concluded that the sedimentary environment is back-arc foreland.
【Fund】: 中国地质调查局重点项目“青藏高原北部空白区基础地质调查与研究”(项目编号1212010310101);; “青藏高原前寒武纪地质古生代构造-古地理综合研究”(项目编号1212010610102)资助
【CateGory Index】: P512.2;TE121.3
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