收稿日期: 2017-03-01
修回日期: 2017-06-11
网络出版日期: 2017-07-10
基金资助
国家科技重大专项（编号：2011ZX05009-003）资助.
Strata sequence and its mechanisms of the Bachu Formation in the Hudson area，Tarim Basin
Received date: 2017-03-01
Revised date: 2017-06-11
Online published: 2017-07-10
通过研究确定塔里木盆地哈得逊地区巴楚组地层序列类型及其成因机理，解决地层演化和沉积历史的相关争议。通过岩心、测井资料的分析及区域地层对比，确定哈得逊地区巴楚组东河砂岩段之上存在下泥岩段和生屑灰岩段。哈得逊地区东河砂岩段、下泥岩段、生屑灰岩段在石炭系早期依次沉积，此沉积序列为该区巴楚组标准沉积序列，该标准序列与塔里木盆地其他地区的东河砂岩段_下泥岩段_生屑灰岩段沉积序列一致。由于在沉积之后即受构造抬升、不均匀剥蚀及混积作用影响，该区大部分巴楚组标准地层序列不再完整，并形成角砾岩段，形成5种地层序列类型（自下而上）：Ⅰ东河砂岩—下泥岩—生屑灰岩；Ⅱ东河砂岩—下泥岩—角砾岩；Ⅲ东河砂岩—下泥岩；Ⅳ东河砂岩—角砾岩；Ⅴ东河砂岩，此种地层序列在东河砂岩油藏区具有明显的分区性。对哈得逊地区巴楚组地层序列的正确认识对该区沉积环境和沉积层序、东河砂岩钙质来源和成岩作用、地震资料应用以及油气勘探等研究具有重要意义。
宁超众，徐怀民，阳建平，孙海航，李维禄，苏琛，陈晓然 . 塔里木盆地哈得逊地区巴楚组地层序列及成因机理[J]. 天然气地球科学, 2017 , 28(7) : 1008 -1019 . DOI: 10.11764/j.issn.1672-1926.2017.06.014
The aim of this article is to confirm the strata sequence and the mechanisms of the Bachu Formation of the Hudson area，Tarim Basin and to settle the related debates of the stratigraphic evolution and sedimentary history.Based on the specific analysis on cores，well-logging and regional stratigraphic correlation，it has been proved that the lower mudstone member and bioclastic limestone member exist above the Donghe sandstone member of the Bachu Formation in Hudson.Donghe sandstone member，lower mudstone member，bioclastic limestone member in Hudson were deposited successively during the Early Carboniferous，which constituted the standard sedimentary sequence of the Bachu Formation in the area.This standard sedimentary sequence is identical with those in other areas in the Trim Basin.Because of the later tectonic uplift，differential denudation and mixed deposition，the strata sequence of the Bachu Formation was no longer intact.The Breccia member was generated and five types of strata sequence were formed (from bottom to top)：Ⅰ Donghe sandstone member-lower mudstone member-bioclastic limestone member，Ⅱ Donghe sandstone member-bioclastic limestone member-breccia member，Ⅲ Donghe sandstone member-lower mudstone member，Ⅳ Donghe sandstone member-breccia member and Ⅴ Donghe sandstone member.Each type of strata sequence lies in its own unique area within the Donghe sandstone reservoir area.The recognition of the Bachu Formation in Hudson influences the study of sedimentary environment and sequence，the source of the calcium of the calcareous interlayers and diagenesis in the Donghe sandstone，the application of the seismic data and the petroleum exploration of the area.
[1]Zhu Huaicheng，Zhang Shiben，Luo Hui，et al.New Advances in the study of the Devonian-Carboniferous boundary in the Tarim Basin[J].Journal of Stratigraphy，2000，24(supplement 1):370-372.[朱怀诚，张师本，罗辉，等.塔里木盆地泥盆系-石炭系界线研究新进展[J].地层学杂志，2000，24(增刊1):370-372.]
[2]Chu Chenglin，Lin Changsong，Zhu Yongfeng，et al.Study on the sequence stratigraphy and depositional system of Donghe sandstone in Tabei Uplift[J].Journal of Southwest Petroleum University:Science & Technology Edition，2011，33(1):15-20.[储呈林，林畅松，朱永峰，等.塔北隆起东河砂岩层序地层和沉积体系研究[J].西南石油大学学报:自然科学版，2011，33(1):15-20.]
[3]Jingyan Liu，Ronald J Steel，Changsong Lin，et al.Geomorphology control on the development of reservoir depositional systems，Devonian Donghetang Formation in the Tabei Uplift of the Tarim Basin，China[J].Marine and Petroleum Geology，2012，38:177 -194.
[4]Guo jianhua，Zeng yunfu，Zhai yonghong，et al.Sequence stratigraphy of Carboniferous Donghe sandstone in Tazhong area，Tarim Basin[J].Acta Petrolei Sinica，1996，23(2):58-66.[郭建华，曾允孚，翟永红，等.塔中地区石炭系东河砂岩层序地层研究[J].沉积学报，1996，23(2):58-66.]
[5]Zhao Jingzhou，Wu Baoguo.Hydrocarbon accumulation mode of Hade 4 Oilfield in Tarim Basin[J].China Peroleum Exploration，2001，6(1):20-23.[赵靖舟，吴保国.塔里木盆地哈得4油田成藏模式探讨[J].中国石油勘探，2001，6(1):20-23.]
[6]Zhao Jingzhou，Tian Jun，Liao Tao，et al.Discovery of Hadexun uplift in the tarim basin and its significance in oil exploration[J].Acta Petrolei Sinica，2002，23(1):27-30.[赵靖舟，田军，廖涛，等.塔里木盆地哈得逊隆起的发现及其勘探意义[J].石油学报，2002，23(1):27-30.]
[7]Wang Zhaoming，Tian Jun，Shen Yinmin，et al.Sedimentary facies of Donghe sandstone during the Late Devonian to Early Carboniferous in Tarim Basin[J].Journal of Palaeogeography，2004，6(3):289-296.[王招明，田军，申银民，等.塔里木盆地晚泥盆世_早石炭世东河砂岩沉积相[J].古地理学报，2004，6(3):289-296.]
[8]Zhu Xiaomin，Zhang Qiang，Lv Xueyan，et al.Comparison of the sedimentary characteristics of the Donghe sandstone sectionbetween the Tabei and Tazhong areas，Tarim Basin[J].Geology in China，2005，32(4):124-130.[朱筱敏，张强，吕雪雁，等.塔里木盆地塔北与塔中地区东河砂岩段沉积特征对比[J].中国地质，2005，32(4):124-130.]
[9]Gu Jiayu，Zhang Xingyang，Guo Bincheng.Characteristics of sedimentation and reservoir of the Donghe sandstone in Tarim Basin and their synthetic analysis[J]，Journal of Palaeogeography，2006，8(3):285-294.[顾家裕，张兴阳，郭彬程.塔里木盆地东河砂岩沉积和储层特征及综合分析[J].古地理学报，2006，8(3):285-294.]
[10]Tan Xiucheng，Chang Yan，Wang Zhenyu，et al.Depositional framework and evolution of Bachu Formation in Tarim Basin[J].Journal of Southwest Petroluem University:Science & Technology Edition，2007，29(4):39-43.[谭秀成，昌燕，王振宇，等.塔里木盆地巴楚组沉积格局与演化[J].西南石油大学学报:自然科学版，2007，29(4):39-43.]
[11]Wu Yinye，Sun Longde，Gu Jiayu，et al.Sedimentary sequence analysis and reservoir evaluation of the Donghe Sandstone of Carboniferous in Manxi area of Tarim Basin[J]，Journal of Palaeogeography:Science & Technology Edition，2008，10(1):13-24.[吴因业，孙龙德，顾家裕，等.塔里木盆地满西地区石炭系东河砂岩沉积层序分析与储集层评价[J].古地理学报:自然科学版，2008，10(1):13-24.]
[12]Zhang Huailiang，Yang Haijun，Shou Jianfeng，et al.Sedimentary periods of Donghe sandstone and hydrocarbon exploration in Tarim Basin[J].Acta Petrolei Sinica，2009，30(6):835-842.[张惠良，杨海军，寿建峰，等.塔里木盆地东河砂岩沉积期次及油气勘探[J].石油学报，2009，30（6):835-842.]
[13]Xu Zhenghua，Ma Qing，Xu Dabao，et al.Donghe sandstone and breccia depositional model discussion of Halahatang region in Tarim Basin[J].Offshore Oil，2010，30(1):26-30.[徐正华，马青，徐大宝，等.哈拉哈塘地区东河砂岩段—角砾岩段沉积模式探讨[J].海洋石油，2010，30(1):26-30.]
[14]Shen Yinmin，Jia Jinhua，Qi Yingmin，et al.Sedimentary facies of Donghe sandstone in the Upper Devonian-Lower Carboniferous and discovery of Hadexun Oilfield in Tarim Basin[J].Journal of Palaeogeography，2011，13(3):279-286.[申银民，贾进华，齐英敏，等.塔里木盆地上泥盆统下石炭统东河砂岩沉积相与哈得逊油田的发现[J].古地理学报，2011，13(3):279-286.]
[15]Xiao Zhaohui，Wang Zhaoming，Wu Jincai，et al.Sequence stratigraphic division and evolution of Carboniferous in Tarim Basin[J].Petroleum Geology & Experiment，2011，33(3):244-248.[肖朝晖，王招明，吴金才，等.塔里木盆地石炭系层序地层划分及演化[J].石油实验地质，2011，33(3):244-248.]
[16]Xin Renchen，Jia Jinhua，Yang Bo.Sequence stratigraphic framework and palaeogeography of the Upper Devonian to Lower Carboniferous in Tarim Basin[J].Journal of Palaeogeography，2011，13(6):665-676.[辛仁臣，贾进华，杨波.塔里木盆地上泥盆—下石炭统层序地层格架与古地理[J].古地理学报，2011，13(6):665-676.]
[17]Yang Bo，Xin Renchen，Jia Jinhua.Sequence stratigraphy and sedimentary evolution of Bachu Formation in Tarim Basin[J].Journal of China University of Mining，2012，41(2):242-255.[杨波，辛仁臣，贾进华.塔里木盆地巴楚组层序地层及沉积演化[J].中国矿业大学学报，2012，41(2):242-255.]
[18]Sun L D，Zhou X Y，Song W J，et al.Donghe Sandstone Subtle Reservoir Exploration and Development Technology in Hade 4 Oilfield[J].Petroleum Science，2004，1(2):35-43.
[19]Xu Huaimin.Fine reservoir Description of the Carboniferous Donghe Sandstone in Hudson[R].Beijing:China University of Petroleum(Beijing)，2006.[徐怀民.哈得逊地区石炭系东河砂岩储层精细描述[R].北京：中国石油大学（北京），2006.]
[20]Lin Changsong.Tectonic Evolution of the Tarim Basin[R].Beijing:China University of Geosciences，2005.[林畅松.塔里木盆地构造演化[R].北京：中国石油大学（北京），2005.]
[21]Ma Qing，Wang Zhenyu，Wang Zhixing，et al.Sedimentary facies of the Carboniferous bioclastic limestone member in Tarim Basin[J].Journal of Southwest Petroleum Institute，2003，25(1):20-24.[马青，王振宇，王兴志，等.塔里木盆地石炭系生屑灰岩段沉积相研究[J].西南石油学院学报，2003，25(1):20-24.]
[22]Lin Changsong，Li Sitian，Liu Jingyan，et al.Tectonic framework and paleogeographic evolution of the Tarim Basin during the Paleozoic major evolutionary stages[J].Acta Petrologica Sinica，2011,27(1):210-218.[林畅松，李思田，刘景彦，等.塔里木盆地古生代重要演化阶段的古构造格局与古地理演化[J].岩石学报，2011，27(1):210-218.]
[23]An Haiting，Li Haiyin，Wang Jianzhong，et al.Tectonic evolution and its controlling on oil and gas accumulation in the Northern Tarim Basin[J].Geotectonicaet Metallogenia，2009，33(1):142-147.[安海亭，李海银，王建忠，等.塔北地区构造和演化特征及其对油气成藏的控制[J].大地构造与成矿学，2009，33(1):142-147.]
[24]Sha Qing’an.Discussion on mixing deposit and hunji rock[J].Journal of Palaeogeography，2001，3(3):63-66.[沙庆安.混合沉积和混积岩的讨论[J].古地理学报，2001，3(3):63-66.]
[25]Zhang Xionghua.Classification and origin of mixosedimentite[J].Geological Science and Technology Information，2000，19(4):31-34.[张雄华.混积岩的分类和成因[J].地质科技情报，2000，19(4):31-34.]
[26]Han Rubing，Liu Qiang，Jiang Tongwen，et al.Feature，origin and distribution of calcareous interlayers:A case of Carboniferous Donghe sandstone in Hade Oilfield，Tarim Basin，NW China[J].Petroleum Exploration and Development，2014，41(4):428-437.[韩如冰，刘强，江同文，等.钙质隔夹层特征、成因及分布——以塔里木盆地哈得油田东河砂岩为例[J].石油勘探与开发，2014，41(4):428-437.]
[27]Zhao Hong，Luo Xiaorong，Xiao Zhongyao，et al.Interlayer features and petroleum geology meaning of Donghe sandstones in the Hadson Oilfield[J].Natural Gas Geoscience，2014，25(6):824-833.[赵洪，罗晓容，肖中尧，等.塔里木盆地哈得逊油田东河砂岩隔夹层特征及其石油地质意义[J].天然气地球科学，2014，25(6):824-833.]
[28]Yang Zhenqiang，Chen Kaixu，Huang Huilan.Carbon isotope in sedimentary strata and new explanation for the origin of ore-bearing anoxic basins[J].Sedimentary Facies and Palaeogeography，1999，19(6):21-28.[杨振强，陈开旭，黄惠兰.沉积地层中成矿作用的碳同位素特征和含矿缺氧盆地成因新观点[J].岩相古地理，1999，19(6):21-28.]
/
| 〈 |
|
〉 |
甘公网安备 62010202000678号