塔里木盆地西南部白垩系-古近系沉积特征与储盖组合

岳勇; 徐勤琪; 傅恒; 席党鹏

doi:10.11781/sysydz201703318

塔里木盆地西南部白垩系-古近系沉积特征与储盖组合

doi: 10.11781/sysydz201703318

1.
中国石化西北油田分公司, 乌鲁木齐 830011
2. 成都理工大学, 成都 610059
3. 中国地质大学, 北京 100083

基金项目: 国家科技重大专项（2011ZX05031-002）资助。

详细信息

作者简介:
岳勇(1980-),男,硕士,工程师,从事塔里木盆地油气地质勘探研究。E-mail:yueyongwjys@sina.com。

中图分类号: TE122.2
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出版历程
- 收稿日期: 2017-01-22
- 修回日期: 2017-04-20
- 刊出日期: 2017-05-28

Reservoir-cap rock assemblage and sedimentary characteristics of Cretaceous-Paleogene in southwestern Tarim Basin

1.
SINOPEC Northwest Oilfield Branch Company, Urumqi, Xinjiang 830011, China
2. Chengdu University of Technology, Chengdu, Sichuan 610059, China
3. China University of Geosciences, Beijing 100083, China

摘要

摘要: 通过对塔里木盆地西南部中新生代地层沉积研究表明，早白垩世继承了侏罗纪的沉积面貌，以陆相沉积占主导，从晚白垩世初到渐新世，受特提斯海洋壳扩张影响，海水多次自西向东侵漫到喀什、叶城及和田等地区，形成了西塔里木海湾。受同期全球海平面整体上升时期大规模海侵影响，塔西南上白垩统-始新统乌拉根组主要发育海相沉积，之后受同期全球海平面整体下降时期海退影响，始新统-渐新统巴什布拉克组为陆相沉积。塔西南晚白垩世-古近纪由于海平面的频繁变化，发育了滨海、浅海-潟湖相的碳酸盐岩、膏盐岩及泥岩沉积体系，形成了上白垩统依格孜牙组碳酸盐岩与上覆古近系阿尔塔什膏盐岩及古近系卡拉塔尔组碳酸盐岩与上覆乌拉根组深色泥岩2套重要的储盖组合，是塔西南地区油气勘探值得重视的重要领域。
- 储盖组合 /
- 沉积特征 /
- 白垩系 /
- 古近系 /
- 塔里木盆地
Abstract: The sedimentary studies of Mesozoic-Cenozoic in the southwestern Tarim Basin indicated that the Early Cretaceous inherited the sedimentary features of the Jurassic, mainly dominated by continental deposits. As the Tethys ocean expanded from the Late Cretaceous to Oligocene, sea water flooded several times to Kashi, Yecheng and Hetian from west to east, forming the West Tarim Bay. Marine facies sedimentation developed from the Upper Cretaceous to the Eocene Wulagen Formation in the southwestern Tarim influenced by large scale transgressions when global sea level rose. After that, continental sedimentation took the leading position from the Eocene to the Oligocene Bashibulake Formation due to global sea level decrease. Sea level changed frequently from the Cretaceous to the Paleogene in the southwestern Tarim, resulting in the preservation of carbonate, gypsum salt and mud rocks of littoral and neritic lagoon facies. There are two sets of reservoir and cap rock assemblages, the one is carbonate rocks in the Upper Cretaceous Yigeziya Formation and gypsum salt rocks in the Paleogene Aertashi Formation, the other is carbonate rocks in the Paleogene Kalataer Formation and dark mudstones in the uplying Wulagen Formation. These two assemblages are important for oil and gas exploration in the southwestern Tarim Basin.
- reservoir and cap rock assemblage /
- sedimentary characteristics /
- Cretaceous /
- Paleogene /
- Tarim Basin

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参考文献(13)

[1]	李滨阳,周瑶琪,吴绍祖,等.塔里木盆地西南依格孜牙组与卡拉塔尔组灰岩碳、氧同位素特征[J].新疆地质,2002,20(S1):88-90. Li Binyang,Zhou Yaoqi,Wu Shaozu,et al.Characteristic of carbon and oxygen isotopes of limestone from Yigeziya and Kalataer formations in southwestern Tarim Basin[J].Xinjiang Geology,2002,20(S1):88-90.
[2]	王琪,陈国俊,薛莲花,等.塔里木西部白垩系-古近系沉积成岩演化特征[J].新疆地质,2002,20(S1):26-30. Wang Qi,Chen Guojun,Xue Lianhua,et al.Sedimentary and diagenetic evolution of the Upper Cretaceous-Eogene controlled by sequence stratigraphy in western Tarim Basin[J].Xinjiang Geo-logy,2002,20(S1):26-30.
[3]	吕海涛,顾忆,丁勇,等.塔里木盆地西南部皮山北新1井白垩系油气成因[J].石油实验地质,2016,38(1):84-90. Lü Haitao,Gu Yi,Ding Yong,et al.Cretaceous petroleum origin in well PSBX1 in the southwestern Tarim Basin[J].Petroleum Geology & Experiment,2016,38(1):84-90.
[4]	何娟,王毅,刘士林,等.塔里木盆地西南坳陷东部构造特征及对油气成藏的控制[J].石油实验地质,2016,38(3):326-332. He Juan,Wang Yi,Liu Shilin,et al.Characteristics of fault structure and its control on hydrocarbon accumulation in the eastern part of southwestern Tarim Basin[J].Petroleum Geology & Experiment,2016,38(3):326-332.
[5]	方爱民,马建英,王世刚,等.西昆仑-塔西南坳陷晚古生代以来的沉积构造演化[J].岩石学报,2009,25(12):3396-3406. Fang Aimin,Ma Jianying,Wang Shigang,et al.Sedimentary tectonic evolution of the southwestern Tarim Basin and west Kunlun Orogen since Late Paleozoic[J].Acta Petrologica Sinica,2009,25(12):3396-3406.
[6]	雍天寿,单金榜,张振春,等.古特提斯海北支:塔里木古海湾岩相古地理[M].北京:科学出版社,1989. Yong Tianshou,Shan Jinbang,Zhang Zhenchun,et al.The north branch of paleotethys:Lithofacies palaeogeography of the Tarim Bay[M].Beijing:Science Press,1989.
[7]	Bosboom R E,Dupont-Nivet G,Houben A J P,et al.Late Eocene sea retreat from the Tarim Basin (West China) and concomitant Asian paleoenvironmental change[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2011,299(3/4):385-398.
[8]	张达景,胡健民,蒙义峰,等.塔里木盆地西南部齐姆根逆冲推覆构造的特征及其与油气的关系[J]. 地质通报,2007,26(3):266-274. Zhang Dajing,Hu Jianmin,Meng Yifeng,et al.Characteristics of Qimugen thrust nappe structure in the southwestern Tarim Basin,Xinjiang,China,and its relationship with hydrocarbon[J].Geological Bulletin of China,2007,26(3):266-274.
[9]	Bosboom R,Dupont-Nivet G,Grothe A,et al.Timing,cause and impact of the Late Eocene stepwise sea retreat from the Tarim Basin (West China)[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2014,403:101-118.
[10]	张英志,林畅松,高志勇,等.塔西南坳陷早白垩世物源体系和沉积古地理分析[J].现代地质,2014,28(4):791-798. Zhang Yingzhi,Lin Changsong,Gao Zhiyong,et al.Depositional paleogeography and provenance analysis of Early Cretaceous southwest depression of Tarim Basin[J].Geoscience,2014,28(4):791-798.
[11]	张亮,韩二斌,朱礼春,等.塔西南坳陷古新统阿尔塔什组蒸发岩沉积旋回特征及控制因素探讨[J].地质学报,2015,89(11):2161-2170. Zhang Liang,Han Erbin,Zhu Lichun,et al.Characteristics of evaporites sedimentary cycles and its controlling factors of Paleocene Aertashi Formation in the Southwestern Tarim Depression[J].Acta Geologica Sinica,2015,89(11):2161-2170.
[12]	周瑞琦,傅恒,徐国盛,等.塔里木盆地周缘洋盆开合在盆地内部的构造沉积响应[J].科学技术与工程,2014,14(35):5-15. Zhou Ruiqi,Fu Heng,Xu Guosheng,et al.The opening-closing of surrounding ocean basin in response to tectonic-sedimentation in Tarim Basin[J].Science Technology and Engineering,2014,14(35):5-15.
[13]	杨海军,沈建伟,张丽娟,等.塔里木盆地西南地区古近系卡拉塔尔组龙介类化石及其古生态[J].中国科学(地球科学),2012,42(11):1634-1646. Yang Haijun,Sheng Jianwei,Zhang Lijuan,et al.Serpulids and their paleoecology of the Paleogene Kalatar Formation in southwest Tarim Basin of China[J].Science China(Earth Sciences),2012,55(7):1087-1100.