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天然气地球科学 ›› 2011, Vol. 22 ›› Issue (2): 315–323.doi: 10.11764/j.issn.1672-1926.2011.02.315

• 天然气地质学 • 上一篇    下一篇

西湖凹陷古近系花港组物源区特征分析

郝乐伟, 刘畅, 王琪, 王欢, 马晓峰, 唐俊, 廖朋   

  1. 1.中国科学院油气资源研究重点实验室,甘肃 兰州730000；
    2.中国科学院研究生院,北京100049；
    3.北京林业大学生物科学与技术学院，北京 100083；
    4.内蒙古科技大学数理与生物工程学院,内蒙古 包头 014010
  • 收稿日期:2010-04-29 修回日期:2010-09-20 出版日期:2011-04-10 发布日期:2011-04-10
  • 通讯作者: 郝乐伟haolewei66@163.com E-mail:haolewei66@163.com
  • 作者简介:郝乐伟(1985-)，男，山东聊城人，博士研究生，主要从事储层沉积学与储层地球化学研究.
  • 基金资助:

    南海深水盆地油气资源形成与分布基础性研究（编号:2009CB219400）;国土资源部全国油气资源战略调查与评价项目“南海北部陆坡深水海域油气资源战略调查与评价”（编号:XQ-2004-05）;国家科技重大专项海洋深水区油气勘探关键技术（编号:2008ZX05000-025）;中国科学院“西部之光”联合学者项目联合资助

Provenance Characteristics of Huagang Formation ( Paleogene) in Xihu Sag, East China Sea

HAO Le-Wei, LIU Chang, WANG Qi, WANG Huan, MA Xiao-Feng, TANG Dun, LIAO Peng-   

  1. 1.Key Laboratory of Petroleum Resources Research,Chinese Academy of Sciences,Lanzhou 730000,China;
    2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China;3.College of Biological Sciences
    and Biotechnology of Beijing Forestry University,Beijing 100083,China;4.School of Mathematics, Physics
    and Biological Engineering of Inner Mongolia University of Science and Technology,Baotou 014010,China
  • Received:2010-04-29 Revised:2010-09-20 Online:2011-04-10 Published:2011-04-10

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摘要：

西湖凹陷花港组是研究区重要的储层之一，其物源一直是争论的焦点。应用砂岩碎屑组分特征，重矿物分析并结合砂地比等值线图精细描绘物源分支，从不同角度、不同层次对西湖凹陷花港组物源体系进行了精细研究。结果表明,西湖凹陷花港组物源主要来自凹陷的西部边缘，东部钓鱼岛隆褶带影响较小，具体分为3大分支:西部的海礁隆起为近物源、西北部虎皮礁凸起和东部钓鱼岛隆褶带物源的结合影响凹陷北部地区、西南部的渔山隆起为凹陷的中南部地区提供物源。通过对岩屑类型、长石特征、石英颗粒和重矿物的微观特征和稀土元素等特征的分析，推测出凹陷周边岩体性质，花港组的母岩主要是岩浆岩，其次为变质岩，沉积岩少见。变质岩主要发育在海礁隆起的中部，影响西部的平湖地区，沉积岩仅在钓鱼岛隆褶带北部地区少量发育。

关键词: 物源分析, 稀土元素配分模式, 重矿物组合, 花港组, 西湖凹陷

Abstract:

The Huagang Formation in Xihu sag is an important reservoir, of which the provenance has been the focus of debate at all times.The source branches are finely pictured according to the characteristics of debris composition and heavy mineral analysis combined with sand percent distribution map.The results show that the Huagang Formation provenance mainly originated from the western edge of Xihu sag and a little from the eastern Diaoyu islands fold belt.The provenance is specific divided into three branches: the western Haijiao uplift source, north-west Hupijiao uplift and east of the Diaoyu islands fold belt source which compensatively affect north area, and south\|west Yushan uplift source affecting the central and southern area.The natures of the rocks around depression are speculated by analyzing debris type, feldspar features, microscopic characteristics of quartz grains and heavy minerals, rare earth elements and so on.The rocks around the Xihu sag are mainly magmatic rocks, secondly metamorphic rocks, and rarely sedimentary rocks.Metamorphic rocks are developed in the middle of Haijiao uplift affecting western Pinghu area.Only a few Sedimentary rocks exit in the northern part of the Diaoyu islands fold belt.

Key words: Provenance analysis, REE distribution pattern, Heavy mineral assemblage, Huagang Formation, Xihu sag

中图分类号: 

  • TE121.3

［1］Fan Dejiang,Sun Xiaogong,Yang Zuosheng.A mathematical model on the quantitative provenance identification:Take the identification of the surface sediment sources from ECS as example［J］.Acta Sedimentologica Sinica,2002,20(1):30-33.［范德江,孙效功,杨作升.沉积物物源定量识别的非线性规划模型——以东海陆架北部表层沉积物物源识别为例［J］.沉积学报,2002,20(1):30-33.］
［2］Yu Hua,Liu Zhenxia,Xiong Yingqian.Provenance study of core DGKS9617 in the East China Sea［J］.Acta Sedimentologica Sinica,2004,22(4):651-657.［余华,刘振夏,熊应乾.东海DGKS9617 岩心物源研究［J］.沉积学报,2004,22(4):651-657.］
［3］Sadooni F N.Stratigraphic sequence,microfacies and petroleum prospects of the Yamama Formation,lower Cretaceous,southern Iraq［J］.AAPG Bulletin,1993,77(11):1971-1988.
［4］Li Zhen,Jiao Yangquan,Liu Chunhua,et al.Source analysis of heavy mineral in Gaoliu area of Huanghua depression［J］.Petroleum Exploration and Development,1998,25(6):5-7.［李珍,焦养泉,刘春华,等.黄骅坳陷高柳地区重矿物物源分析［J］.石油勘探与开发,1998,25(6):5-6.］
［5］Xu Tianwu,Wang Yingmin,Zeng Jianhui,et al.Sedimentary facies and provenance analysis of late Cretaceous Taizhou Formation in Gaoyou-Haian depression,north Jiangsu(Subei)basin［J］.Acta Geoscientica Sinica,2007,28(6):627-634.［徐田武,王英民,曾溅辉,等.苏北盆地高邮—海安地区晚白垩世泰州组沉积相及物源分析［J］.地球学报,2007,28(6):627-634.］
［6］Zhang Fushun.Fan delta and braided delta sediments in Baiyinchagan depression［J］.Acta Geoscientica Sinica,2005,26(6):553-556.［张福顺.白音查干凹陷扇三角洲与辫状河三角洲沉积［J］.地球学报,2005,26(6):553-556.
［7］Wu Fadong,Lu Yongchao,Ruan Xiaoyan.Application of heavy minerals cluster analysis to study of clastic sources and stratigraphic correlation［J］.Geoscience,1996,10(3):397-403.［武法东,陆永潮,阮小燕.重矿物聚类分析在物源分析及地层对比中的应用——以东海陆架盆地西湖凹陷平湖地区为例［J］.现代地质,1996,10(3):397-403.］
［8］Liu Jianjun,Chen Kaiyuan,Shi Zhongsheng,et al.Provenance characters of Paleogene in Xihu sag in East China Sea basin［J］.Science & Technology Progress and Policy,2003,(supplement):241-242.［刘建军，陈开远，史忠生,等.东海陆架盆地西湖凹陷下第三系物源分析［J］.科技进步与对策,2003,（增刊）:241-242.］ 
［9］Zhang Daofeng,Yang Wenjing,Qi Yaling，et al.Analysis of the material source of upper Paleozoic Shanxi Formation in Shenmu region of Ordos basin［J］.Natural Gas Geoscience,2009,20(6):902-906.［张道锋,杨文敬,漆亚玲,等.鄂尔多斯盆地神木地区上古生界山西组物源分析［J］.天然气地球科学,2009,20(6):902-906.］
［10］Dickinson W R.Interpreting Provenance Relations from Detrital Modes of Sandstones［M］// Zuffa G Ged.Provenance of Arenites.Dordrecht:D.Reidel,NATO-ASI,Series 1,1985,48:333-361.
［11］Li Zhong,Sun Shu,Li Renwei,et al.Mesozoic filling sequence and its indication to Dabieshan orogeny in Hefei basin［J］.Science in China:Series D,2000,30(3):256-263.［李忠,孙枢,李任伟,等.合肥盆地中生代充填序列及其对大别山造山作用的指示［J］.中国科学:D辑,2000，30(3):256-263.］
［12］Liu Rui′e,Wei Xiaofeng,Wang Yali,et al.The geochemical characteristics of rare earth elements of the shale rock in the gologic signification of the analysis of the sedimentary provenace:An example in the upper Palaeozoic in the Ordos basin［J］.Natural Gas Geoscience,2005,16(6):788-791.［刘锐娥,卫孝峰,王亚丽,等.泥质岩稀土元素地球化学特征在物源分析中的意义——以鄂尔多斯盆地上古生界为例［J］.天然气地球科学,2005,16(6):788-791.］
［13］Xie Xiaojun,Deng Hongwen.Controls of the transverse accommodation zones on the provenance system in Baxian sag［J］.Natural Gas Geoscience,2008,19(3):334-338.［谢晓军,邓宏文.冀中坳陷霸县凹陷横向调节带对物源体系的控制作用［J］.天然气地球科学,2008,19(3):334-338.］
［14］Zhao Hongge,Liu Chiyang.Approaches and prospects of provenance analysis［J］.Acta Sedimentologica Sinica,2003,21(3):409-415.［赵红格,刘池洋.物源分析方法及研究进展［J］.沉积学报,2003,21(3):409-415.］
［15］Li Xiaolan.Discovery course of oil and gas in Xihu trough,the East China Sea shelf basin［J］.Offshore Oil,2007,27(2):14-17.［李晓兰.东海陆架盆地西湖凹陷油气发现历程回顾［J］.海洋石油,2007,27(2):14-17.］
［16］Yan Wentao.Analysis of Sedimentary Facies on the Huagang Formation of the Oligocene in the Xihu Sag of the East China Sea Shelf Basin［D］.Qingdao:Ocean University of China,2007:7-8.［颜文涛.东海陆架盆地西湖凹陷渐新统花港组沉积相分析［D］.青岛:中国海洋大学，2007:7-8.］
［17］Xiao Jianxin,Sun Fenjin,He Naixiang,et al.Permian Shanxi Formation and Member 8 of Xiashihezi Formation in Ordos basin:Palaeogeography and catchment area for sediments derived from north and south provenances［J］.Journal of Palaeogeograph,2008,10(4):341-354.［肖建新,孙粉锦,何乃祥,等.鄂尔多斯盆地二叠系山西组及下石盒子组盒8段南北物源沉积汇水区与古地理［J］.古地理学报,2008,10(4):341-354.］
［18］Wang Changyong,Zheng Rongcai,Wang Haihong,et al.Provenance analysis of Chang-6 oil reservoir set in Jiyuan region in Ordos basin［J］.Acta Sedimentologica Sinica,2008,26(6):52-58.［王昌勇,郑荣才,王海红,等.鄂尔多斯盆地姬塬地区长6油层组物源分析［J］.沉积学报,2008,26(6):52-58.］
［19］Yang Shouye,Li Congxian.Research progress in ree trace for sediment source［J］.Advance in Earth Sciences,1999,14(2):164-166.［杨守业,李从先.REE示踪沉积物物源研究进展［J］.地球科学进展,1999,14(2):164-166.］
［20］Byrne H，Kimk H.Rare earth element scavening in sea water［J］.Geochim.Acta,1990,54(2):645-656.
［21］Allègre C J,Michard G.Introduction to Geochemistry:Geophysics and Astrophysics Monographs［M］.Kluwer:Academic Publishers,1974.
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