|Table of Contents|

Q-clustering Analysis for Relationship Among Multiple Energy Mineral Deposits in Ordos Basin(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2010年第01期
Page:
48-53
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Q-clustering Analysis for Relationship Among Multiple Energy Mineral Deposits in Ordos Basin
Author(s):
PAN Ai-fang1; 2;  WANG Fang-yi3;  ZHANG Dao-fa3;  HE Ying4
(1.School of Earth Sciences and Resources, Chang'an University, Xi'an 710054, Shaanxi, China; 2.Key Laboratory of Western Mineral Resources and Geological Engineering of Ministry of Education,Chang'an University, Xi'an 710054, Shaanxi, China; 3.The Fifth Oil Production Factory, Changqing Oilfield Company, China National Petroleum Corporation, Xi'an 710021, Shaanxi,China; 4.Department of Geology, Northwest University, Xi'an 710069, Shaanxi, China)
Keywords:
Ordos Basin;  Q-clustering;  fluid;  energy mineral deposit
PACS:
P595;P618
DOI:
-
Abstract:
In order to reveal the relationship among multiple energy mineral deposits in Ordos Basin, the contents of 57 elements of the oil, oilfield water and the chloroform bitumen of coal, gangue, uranium deposit and their wall rock was calculated by Q-clustering.The results showed that genetic features of the oil with Lower Jurassic Yan'an Formation and Middle Jurassic Zhiluo Formation and the petroleum asphalt with Triassic Yanchang Formation was similar; the petroleum asphalt of Triassic Yanchang Formation, the asphalt in oil sandstones of Triassic Yanchang Formation and the petroleum asphalt of Middle Jurassic Zhiluo Formation had similar genetic features; the coal asphalt of Lower Jurassic Yan'an Formation in Shenmu and Middle Iurassic Zhiluo Formation in Dongsheng, the petroleum and coal asphalt in the coal bed of Lower Jurassic Yan'an Formation in Chenjiashan of Tongchuan had similar genetic features; the petroleum asphalt in the coal bed of Lower Jurassic Yan'an Formation in Chenjiashan of Tongchuan was in connection with the coal asphalt of Permo Carboniferous in Heidaigou of Jungar; the petroleum asphalt of Lower Jurassic Yan'an Formation was closely related with the enrichment of uranium mineralization; the origin of natural gas was complicated, and related with the further evolvement of petroleum and coal.The origin of multiple energy mineral deposit was complicated, correlative and the mineralization/reservoiring was multi-source in Ordos Basin.

References:

[1] 涂光炽.成煤、成油、成气、成盐和成金属矿之间的关系[J].有色金属矿产与勘查,1994,3(1):1-3.
[2] 刘池洋.沉积盆地动力学与盆地成藏(矿)系统[J].地球科学与环境学报,2008,30(1):1-23.
[3] Bazhenova O K,Arefiev O A,Frolov E B.Oil of the Volcano Uzon Caldera,Kamchatka[J].Organic Geochemistry,1998,29(1/3):421-428.
[4] Clifton C G,Walters C C,Simoneit B R T.Hydrothermal Petroleums from Yellowstone National Park,Wyoming,USA[J].Applied Geochemistry,1990,5(1/2):169-191.
[5] Czochanska Z,Sheppard C M,Weston R J,et al.Organic Geochemistry of Sediments in New Zealand,PartⅠ:a Biomarker Study of the Petroleum Seepage at the Geothermal Region of Waiotapu[J].Geochimumica et Cosmochimica Acta,1986,50(4):507-515.
[6] Tiercelin J J,Thouin C,Kalala T,et al.Discovery of Sublacustrine Hydrothermal Activity and Associated Massive Sulfides and Hydrocarbons in the North Tanganyika Trough,East African Rift[J].Geology,1989,17(11):1053-1056.
[7] 刘池洋,谭成仟,孙 卫,等.多种能源矿产共存成藏(矿)机理与富集分布规律研究[C]∥刘池洋.盆地多种能源矿产共存富集成藏(矿)研究现状.北京:科学出版社,2005:1-16
[8] 钟宁宁,陈恭洋.煤系气油比分配控制因素及其与大中型气田的关系[M].北京:石油工业出版社,2002.
[9] 李荣西.九十年代煤系烃源岩研究新进展[J].地质科技情报,2000,19(4):55-59.
[10] 张祖还.铀地球化学[M].北京:原子能出版社,1984.
[11] Spirakis C S.The Roles of Organic Matter in the Formation of Uranium Deposits in Sedimentary Rocks[J].Ore Geology Review,1996,11(1/3):53-69.
[12] Meunier J D,Landais P,Pagel M.Experimental Evidence of Uraninite Formation from Diagenensis of Uranium-rich Organic Matter[J].Geochimica et Cosmochimica Acta,1990,54(3):809-817.
[13] 杜乐天.盆地矿套[J].国外铀金地质,2002,19(3):140-146.
[14] 陈建渝,朱芒征.含油气系统与有机地球化学的关系[J].石油与天然气地质,1999,20(3):246-249.
[15] 李贤庆,侯读杰,张爱云,等.鄂尔多斯中部奥陶系水溶烃的分子地球化学特征[J].沉积学报,2002,20(4):710-715.
[16] 朱西养,汪云亮,王志畅,等.东胜砂岩型铀矿微量元素地球化学特征初探[J].地质地球化学,2003,31(2):39-45.
[17] 潘爱芳,马润勇,黎荣剑.鄂尔多斯盆地深部流体地球化学研究[M].北京:石油工业出版社,2006.
[18] 赵文智,胡素云,王泽成,等.鄂尔多斯盆地基底断裂在上三叠统延长组石油聚集中的控制作用[J].石油勘探与开发,2003,30(5):1-5.
[19] 王庭斌.新近纪以来中国构造演化特征与天然气田的分布格局[J].地学前缘,2004,11(4):403-416.
[20] 邸领军,张东阳,王宏科.鄂尔多斯盆地喜山期构造运动与油气成藏[J].石油学报,2003,24(2):34-37.
[21] 马润勇,彭建兵,袁志东,等.青藏高原隆升的黄土高原构造侵蚀效应[J].地球科学与环境学报,2007,29(3):289-293.
[22] 赵 虹,党 犇,陈永胜,等.鄂尔多斯盆地姬塬地区三叠系延长组长2油层组储层特征及影响因素[J].西安科技大学学报,2009,29(5):579-583.
[23] 陈永胜,赵 虹,郑小杰,等.鄂尔多斯盆地志丹探区延长组储层特征研究及评价[J].西北地质,2009,42(2):83-88.
[24] 白清华,柳益群,樊婷婷.鄂尔多斯盆地上三叠统延长组浊沸石分布及其成因分析[J].西北地质,2009,42(2):100-107.
[25] 郝世彦,魏仙样,魏建设.志丹油田寨科区延长组长2油层储集条件研究[J].西北地质,2009,42(3):86-94.
[26] 顾雪祥,王 乾,付绍洪,等.分散元素超常富集的资源与环境效应:研究现状与发展趋势[J].成都理工大学学报:自然科学版,2004,31(1):15-21.
[27] 邓 军,陈学明,饶轶群,等.南岭地区两种类型盆地的压实流体系统及其矿化作用[J].现代地质,2004,18(1):1-7.
[28] 潘爱芳,赫 英,徐宝亮,等.鄂尔多斯盆地基底断裂地球化学特征研究[J].西北大学学报:自然科学版,2005,35(4):440-444.
[29] 潘爱芳,赫 英,黎荣剑,等.鄂尔多斯盆地基底断裂与能源矿产成藏成矿的关系[J].大地构造与成矿学,2005,29(4):459-464.
[30] 潘爱芳,赫 英,黎荣剑.鄂尔多斯盆地能源矿产氯仿沥青Sm-Nd同位素研究[J].中国地质,2007,34(3):440-444.

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Last Update: 2010-03-20