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《Acta Sedimentologica Sinica》 2010-05
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Permian Lacustrine Eruptive Hydrothermal Dolomites,Santanghu Basin,Xinjiang Province

LIU Yi-qun1 LI Hong1 ZHU Yu-shuang1 HU Ting2 FU Guo-bin2 LIU Hong-fu1ZHOU Xiao-hu1 ZHENG Chao-yang1 FAN Ting-ting1(1.State Key Laboratory of Continental Dynamics,Northwest University,Department of Geology,Northwest University,Xi'an 710069;2.Exploration Development & Research Institute of Tu-HA Oilfield,CNPC,Hami Xinjiang 830002)  
Late Carboniferous to Early Permian was an important period of tectonic changes and ocean-continent transformation in northern Xinjiang area.Several approximately east-west intracontinental rifts occurred,such as Santanghu basin,where abundant basic,intermediate,and acidic volcanic rocks are present.Deposition of moderately deep lacustrine sediments of the Lucaogou Formation occurred during Middle Permian in Northern Xinjiang.The sediments include thick dark colored shale,tuffaceous shale,and dolomite shale,intercalated with dolomitic micritic limestone,tuff,dolomite,and volcanic rocks.They contain Turfania,bivalve,conchostracans,and ostracoda.The dolomite is composed of interlaminated ankerite,cryptocrystalline quartz and organic matter including algae,and analcime laminae as annalcite.The analcites were cenmented and replaced by ankerite.In addition,hydrothermal minerals like albite,illite,anhydrite,and pyrite are present.These hydrothermal minerals were firstly recognized in the Lucaogou,and the distribution of dolomite is consistent with that of the underlying Upper Carboniferous volcanic rocks,which occur in fractures and point sources.The network-like and branch-like fractures in volcanic rocks with a brecciated structure are filled with hydrothermal minerals indicating deposition around a hydrothermal vent.Preliminary analysis indicateds that dolomites were related to magmatism and mantle hydrothermal fluid,and formed as lacustrine eruptive hydrothermal dolomites.
【Fund】: 《中国西北地区构造—岩相古地理研究与编图》(批准号:YPH08103);; 国家自然科学基金青年科学基金项目(批准号:40802024)联合资助
【CateGory Index】: P588.245
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【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 TIAN Jing chun 1, ZENG Yun fu 1, ZHENG He rong 2, KONG Fan xian 2, FENG You liang 2 (1.Chengdu Univresity of Technology, China; 2.Geologial Scientific Research Institute of Shengli Petroleum Administrative Bureau);THE RESEARCH OF THE RESERVOIR CHARACTERISTICS OF THE DOLOSTONE INTERCALATED IN MUDSTONE IN TERRIGENOUS OIL BEARING BASIN ——Taking the dolostone on the upper of Sha Ⅲ in Dongying sag as an example[J];JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY;2000-01
2 PANG Yan chun, LIN Li, ZHU Li dong, CHEN Zhi gang, LI Yi min, XIONG Yong zhu, FU Xiu gen (Chengdu University of Technology, China);RESEARCH ADVANCES IN HYDROTHERMAL VENT COMMUNITIES[J];Journal of Chengdu University of Technology;2002-04
3 ZHENG Rong cai 1, WANG Cheng shan 1, ZHU Li dong 1, LIU Hong jun 1, FANG Guo yu 2, DU Wen bo 2, WANG Chong xiao 2, WANG Man fu 2 (1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, China; 2.Research Institute of Yumen Oil Field Branch Company);DISCOVERY OF THE FIRST EXAMPLE OF "WHITE SMOKE TYPE" OF EXHALATIVE ROCK (HYDROTHERMAL SEDIMENTARY DOLOSTONE) IN JIUXI BASIN AND ITS SIGNIFICANCE[J];Journal of Chengdu University of Technology(Science & Technology Edition);2003-01
4 Lan Jianghua (Chengdu University of Technology, China);THE GENETIC MODEL OF PALEODISSOLUTION CONTROLLED RESERVOIR OF CARBONIFEROUS SYSTEM IN THE DACHIGANJING TECTONIC BELT,SICHUAN BASIN[J];JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY;1999-01
5 Shi Ji'an (Lanzhou Institute of Geology ,Chinese Academy of Sciences);The Origin of Dolostone and Its Reservoir Characteristics of Sinian and Palaeozoic,Northwestern Margin of Tarim Basin[J];Acta Sedimentologica Sinica;1993-02
6 Zhang Xiaobao (Lanzhou Institute of Geology,Chinese Academy of Sciences);Study on the Origin of the Dolostone Intercalcated in the Black Shales in Middle Permian Lucaogou Formation Eastern Part of Southern Margin of Junggar Basin[J];Acta Sedimentologica Sinica;1993-02
7 JIN Zhen kui FENG Zeng zhao (University of Petroleum Beijing 102200);Origin of Dolostones of the Lower Permian in East Yunnan—West Sichuan ——Dolomitization through Leaching of Basalts[J];ACTA SEDIMENTOLOGICA SINICA;1999-03
8 YUAN Jing 1 ZHAO Cheng Ling 2 ZHANG Shan Wen 3 1(University of Petroleum,Dongying Shandong 257062) 2(University of Petoleum,Changping Beijing 022000) 3(Institute of geology of Shengli Oil Bureau,Dongying,Shandong 257000);Genetic Model of the Deep Water Salt Lake of the Paleogene Sha-4 Member in Dongying Sag[J];ACTA SEDIMENTOLOGICA SINICA;2000-01
9 CHEN Fa liang 1 ZHU Hui 2 LI Xu tao 1 MIAO Cui zhi 1 1(Survey Institute of Geology, Zhongyuan Petroleum Exploration Bureau, Puyang Henan 457001) 2(Institute of Exploration and Development Zhongyuan Oilfield,Puyang Henan 457001);Partition of Sequence Strata and Discussion about Salt-rock Resource in Shahejie Formation of Eogene, Dongpu Depression[J];ACTA SEDIMENTOLOGICA SINICA;2000-03
10 ZHANG Yong sheng (Laboratory of Salt Lake Resources and Environment, Institute of Mineral Deposits,Chinese Academy of Geological Sciences,Beijing 100037);Mechanism of Deep Burial Dolomitization of Massive Dolostones in the Middle Majiagou Group of the Ordovician,Ordos Basin[J];ACTA SEDIMENTOLOGICA SINICA;2000-03
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