吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (5): 1310-1321.doi: 10.13278/j.cnki.jjuese.201505105

• 地质与资源 • 上一篇    下一篇

羌塘盆地东部中侏罗统陆源碎屑与碳酸盐混合沉积成岩特征

马伯永1, 王根厚2, 李尚林3, 徐红燕1   

  1. 1. 中国地质调查局, 北京 100037;
    2. 中国地质大学(北京)地球科学与资源学院, 北京 100083;
    3. 中国地质调查局西安地质调查中心, 西安 710054
  • 收稿日期:2014-02-21 发布日期:2015-09-26
  • 作者简介:马伯永(1972),男,高级工程师,博士,主要从事地层学及区域地质研究,E-mail:mby562@126.com。
  • 基金资助:

    国家自然科学基金项目(40172014);中国地质调查局区域地质调查项目(I46C004003)

Characteristics of Mixed Sedimentations and Diagenesis of Terrigenous Clastic Rock and Carbonate:The Middle Jurassic in the East Qiangtang Basin, Tibet, China

Ma Boyong1, Wang Genhou2, Li Shanglin3, Xu Hongyan1   

  1. 1. China Geological Survey, Beijing 100037, China;
    2. College of Geoscience and Mineral Resources, China University of Geosciences, Beijing 100083, China;
    3. Xi'an Center of China Geological Survey, China
  • Received:2014-02-21 Published:2015-09-26

摘要:

近年来,混合沉积显示的沉积环境和油气地质意义越来越受到学界的重视。羌塘盆地是目前国内油气勘探最重要的战略选区之一,具有良好的油气勘探远景。研究区侏罗系广泛发育陆源碎屑与碳酸盐的混合沉积。综合前人研究成果、区域地质资料和室内样品分析,笔者对研究区广泛分布混合沉积的岩石学特征、沉积环境、成岩作用进行了详细地研究。研究发现:区内中侏罗统混合沉积表现为混积岩、混积层系两种形式;对岩性、层系及组合特征进行观察发现,它们主要形成于滨岸、碳酸盐岩缓坡、潮坪沉积环境,把混合沉积划分为4个三级地层层序,提高了地层划分的精度,建立了研究区中侏罗世雀莫错期、布曲期、夏里期的岩相古地理格局;混积岩中最显著的成岩作用类型有压实-压溶、胶结、破裂和溶蚀作用,其中以破裂作用、溶蚀作用最为发育,有利于形成优质储层,可为沉积储层预测及研究区的石油普查评价提供重要参考。

关键词: 碳酸盐岩, 陆源碎屑岩, 混合沉积, 成岩作用, 油气, 中侏罗统, 羌塘盆地

Abstract:

Geological researchers have paid more and more attention to the mixed siliciclastic carbonate sediments and its geological significance of oil and gas. Qiangtang basin is one of the most important strategic selection for oil and gas exploration. The mixed siliciclastic carbonate sediments are extensively developed in the eastern part of Qiangtang basin. Combined the regional geological data and indoor sample analysis with the previous researches, we study the characteristics of the mixed sediments, their sedimentary environment, and their diagenesis. The results show that the research area is characterized by interactive sediments of terrigenous clast and carbonate on the microscopic level, so called "mixed rock", and by interbedded rocks of terrigenous clastic rock, carbonate rock or mixed rock in macro. These lithoface types are mainly formed in a sedimentary environment of shore, carbonate ramp, or tidal flat-lagoon. It can be divided into four three-level sequences, which remarkably improves the precision of stratigraphic classification. The lithofacies palaeogeography of Quemocuo, Buqu and Xiali age are established. The diagenesis types of the mixed rocks are cementation, compaction, pressure solution, fragmentation, and dissolution. The pressure solution, fragmentation and dissolution are more common than others, which are conducive to form a mixed rock reservoir. This research can provide valuable information for petroleum and natural gas exploration.

Key words: carbonate rock, terrigenous clastic rock, mixed sedimentation, diagenesis, oil and gas, Middle Jurassic, Qiangtang basin

中图分类号: 

  • P618.13

[1] Mount J F. Mixing of Ciliciclastic and Carbonate Sediments in Shallow Shelf Environments[J].Geology,1984, 2(7):432-435.

[2] 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. Sha Qing'an. Discussion on Mixing Deposit and Hunji Rock[J]. Journal of Palaeogeography,2001,3(3):63-66.

[3] 张锦泉,叶红专.论碳酸盐与陆源碎屑的混合沉积[J].成都地质学院学报,1989,16(2):87-92. Zhang Jinquan, Ye Hongzhuan. Study on Carbonate and Siliciclastic Mixed Sediments[J]. Journal of Chengdu College of Geology, 1989, 16(2):87-92.

[4] 冯近来,曹剑,胡凯, 等.陆源碎屑与碳酸盐混积岩及其油气地质意义[J].高校地质学报,2011,17(2) 297-307. Feng Jinlai, Cao Jian, Hu Kai,et al. A Review on Mixed Rocks of Terrigenous Clastics and Carbonates and Their Petroleum-Gas Geological Significance[J]. Geological Journal of China Universities,2011,17(2) 297-307.

[5] Palermol D, Aigner1 T, Geluk M, et al. Reservoir Potential of a Lacustrine Mixed Carbonate/Siliciclastic Gas Reservoir:The Lower Triassic Rogenstein in the Netherlands[J]. Journal of Petroleum Geology,2008, 31(1): 61-96.

[6] Bech stǎdt T, Schweizer T. The Carbonate-Siliciclastic Cycles of the East-Alpine Raibl Group: Result of Third-Order Sea-Level Fluctuations in the Carnian[J]. Sedimentary Geology,1991,70: 241-270.

[7] Best M M R,Kidwell S M. Bivalve Taphonomy in Tropical Mixed Siliciclastic-Carbonate Settings:I:Environmental Variation in Shelf Condition[J]. Paleobiology,2000,26(1): 80-102.

[8] Brook s G R,Doyle L J,Suthard B C,et al. Facies Architecture of the Mixed Carbonate/Siliciclastic Inner Continental Shelf of Westcentral Florida: Implications for Holocene Barrier Development[J].Marine Geology, 2003, 200: 325-349.

[9] Campbell A E. Shelf-Geometry Response to Changes in Relative Sea Level on a Mixed Carbonate-Siliciclastic Shelf in the Guyana Basin[J]. Sedimentary Geology,2005, 175: 259-275.

[10] Coffe y B P, Read J F. Mixed Carbonate-Siliciclastic Sequence Stratigraphy of a Paleogene Transition Zone Continental Shelf, Southeastern USA[J]. Sedimentary Geology,2004,166: 21-57.

[11] El-Azabi M H, El-Araby A. Depositional Framework and Sequence Stratigraphic Aspects of the Coniacian-Santonian Mixed Siliciclastic/Carbonate Matulla Sediments in Nezzazat and Ekma Blocks, Gulf of Suez, Egypt[J]. Journal of African Earth Sciences, 2007,47: 179-202.

[12] Khetani A B, Read J F. Sequence Development of a Mixed Carbonate-Siliciclastic High-Relief Ramp, Mississippian, Kentucky, USA[J]. Journal of Sedimentary Research,2002,72(5): 657-672.

[13] LaGesse J, Read J F. Up Dip Sequence Development on a Wave and Current-Dominated Mixed Carbonate-Siliciclastic Continental Shelf: Paleogene,North Carolina,Eastern USA[J]. Sedimentary Geology,2006,184:155-182.

[14] 张茂恒, 孔兴功.江苏盱眙震旦纪混合沉积体系的特征[J].吉林大学学报:地球科学版,2011,47(5):1448-1457. Zhang Maoheng,Kong Xinggong.Characteristics of Simian Mixing Sedimentary System in Xuyi, Jiangsu Province of China[J] . Journal of Jinlin University: Earth Science Edition,2011,41(5):1448-1457.

[15] 贾建称,吴新国,王根厚,等.羌塘盆地东部中生代沉积特征与构造演化[J].中国地质,2006,33(5) 999-1004. Jia Jiancheng, Wu Xinguo, Wang Genhou, et al. Mesozoic Sedimentary Characteristics and Tectonic Evolution in the Eastern Part of the Qiangtang Basin[J]. Geology in China,2006,33(5): 999-1004.

[16] 马伯永.青藏高原羌塘盆地东部侏罗统碳酸盐与陆源碎屑混合沉积体系研究[D]. 北京: 中国地质大学,2011. Ma Boyong. A Study of the Middle Jurassic Mixed Siliciclastic and Carbonate Sedimentary System in the Eastern part of the Qiangtang Basin, Tibet[D]. Beijing: China University of Geosciences, 2011.

[17] 张雄华. 混积岩的分类和成因[J]. 地质科技情报, 2000,19(4): 31-34. Zhang Xionghua. Classification and Origin of Mixosedimentite[J].Geological Science and Technology Information,2000,19(4):31-34.

[18] 董桂玉,陈洪德,何幼斌,等.陆源碎屑与碳酸盐混合沉积的几点思考[J].地球科学进展, 2007,22(9):931-939. Dong Guiyu,Chen Hongde,He Youbin,et al. Some Problems on the Study of the Mixed Siliciclastic Carbonate Sediments[J].Advances in Earth Research, 2007,22(9): 931-939.

[19] 李忠,韩澄林,寿建峰. 沉积盆地成岩作用系统及时空属性[J].岩石学报, 2006, 22(8):2151-2164. Li Zhong, Han Chenglin, Shou Jianfeng. Diagenesis Systems and Theirspatio-Temporal Attributes in Sedimentary Basins[J]. Acta Petrologic Sincia,2006,22(8): 2151-2164.

[20] 钟大康,朱筱敏,张琴.不同埋深条件下砂泥岩互层中砂岩储层物性变化规律[J].地质学报,2004,78(6): 863-871. Zhong Dakang, Zhu Xiaomin, Zhang Qin. Variation Characteristics of Sandstone Reservoirs When Sandstone and Mudstone Are Interbedded at Different Buried Depths[J] . Acta Geologica Sinica,2004,78(6): 863-871.

[1] 牟敦山, 付广, 陈雪晴. 南堡1号构造馆三段断盖配置油气渗漏部位及其控藏作用[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1008-1017.
[2] 陈爱民. 澳大利亚Bonaparte盆地WA-406-P区块油气成藏条件及控制因素[J]. 吉林大学学报(地球科学版), 2018, 48(4): 965-980.
[3] 林敉若, 操应长, 葸克来, 王健, 陈洪, 吴俊军. 阜康凹陷东部斜坡带二叠系储层特征及控制因素[J]. 吉林大学学报(地球科学版), 2018, 48(4): 991-1007.
[4] 李文强, 郭巍, 孙守亮, 杨绪海, 刘帅, 侯筱煜. 塔里木盆地巴楚—麦盖提地区古生界油气藏成藏期次[J]. 吉林大学学报(地球科学版), 2018, 48(3): 640-651.
[5] 孙海涛, 钟大康, 李勇, 毛亚昆, 杨宪彰. 超深低孔特低渗砂岩储层的孔隙成因及控制因素——以库车坳陷克深地区巴什基奇克组为例[J]. 吉林大学学报(地球科学版), 2018, 48(3): 693-704.
[6] 舒晴, 朱晓颖, 高维, 李瑞, 尹航. 三塘湖盆地航磁异常特征及油气远景预测[J]. 吉林大学学报(地球科学版), 2018, 48(2): 451-460.
[7] 姚刚, 董向欣, 李丽丽, 马国庆, 孟令顺. 东海陆架盆地构造划分的高精度重磁解释技术[J]. 吉林大学学报(地球科学版), 2018, 48(2): 517-524.
[8] 李昂, 鞠林波, 张丽艳. 塔里木盆地古城低凸起古-中生界构造演化特征与油气成藏关系[J]. 吉林大学学报(地球科学版), 2018, 48(2): 545-555.
[9] 杨德相, 付广, 孙同文, 李熹微, 姜海燕, 刘滨莹. 油源断裂优势通道输导油气能力综合评价方法及其应用[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1678-1686.
[10] 马德龙, 何登发, 魏东涛, 王彦君, 魏彩茹. 准噶尔盆地南缘古牧地背斜多期构造变形特征[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1695-1704.
[11] 张焕旭, 陈世加, 路俊刚, 刘超威, 陈娟, 李勇, 徐坤. “膨胀力”作用下致密砂岩储层石油运聚特征[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1341-1351.
[12] 刘鑫金, 冯阵东, 李聪, 周艳, 王亚明. 近源湖盆砂砾岩储层次生溶孔成因探讨——以查干凹陷祥6井区为例[J]. 吉林大学学报(地球科学版), 2017, 47(2): 393-404.
[13] 张博为, 付广, 张居和, 胡明, 刘峻桥, 王浩然. 油源断裂转换带裂缝发育及其对油气控制作用——以冀中坳陷文安斜坡议论堡地区沙二段为例[J]. 吉林大学学报(地球科学版), 2017, 47(2): 370-381.
[14] 范卓颖, 林承焰, 鞠传学, 韩长城, 熊陈微. 塔河油田二区奥陶系优势储集体特征及控制因素[J]. 吉林大学学报(地球科学版), 2017, 47(1): 34-47.
[15] 牛君, 黄文辉, 丁文龙, 蒋文龙, 张亚美, 漆立新, 云露, 吕海涛. 麦盖提斜坡奥陶系碳酸盐岩碳氧同位素特征及其意义[J]. 吉林大学学报(地球科学版), 2017, 47(1): 61-73.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!