三塘湖盆地马朗凹陷石炭系火山岩系烃源岩识别与预测

柳波; 贾梦成; 黄志龙; 陈旋; 申英; 吴红烛

doi:10.11781/sysydz201504452

三塘湖盆地马朗凹陷石炭系火山岩系烃源岩识别与预测

doi: 10.11781/sysydz201504452

柳波^1,2,
贾梦成^1,2,
黄志龙³,
陈旋⁴,
申英⁴,
吴红烛³

1.
东北石油大学非常规油气成藏与开发省部共建国家重点实验室培育基地, 黑龙江大庆 163318
2. 黑龙江省高等学校科技创新团队"断裂变形、封闭性及与流体运移", 黑龙江大庆 163318
3. 中国石油大学油气资源与探测国家重点实验室, 北京 102249
4. 中国石油吐哈油田公司勘探开发研究院, 新疆哈密 839009

基金项目: 国家自然科学基金项目(41472125)、国家青年自然科学基金(41202101)、中国博士后科学基金(2013M541338)和黑龙江省教育厅科学技术研究项目(12541084)联合资助。

详细信息

作者简介:
柳波(1983-),男,博士,副教授,从事油气成藏地质学、非常规油气地质与勘探。E-mail:liubo6869@163.com。

中图分类号: TE122.1
计量
- 文章访问数: 1086
- HTML全文浏览量: 55
- PDF下载量: 961
- 被引次数: 0
出版历程
- 收稿日期: 2014-05-18
- 修回日期: 2015-05-06
- 刊出日期: 2015-07-28

Identification and prediction of source rocks in Carboniferous volcanic systems in Malang Sag, Santanghu Basin

1.
Accumulation and Development of Unconventional Oil and Gas, State Key Laboratory Cultivation Base Jointly-constructed by Heilongjiang Province and Ministry of Science and Technology, Northeast Petroleum University, Daqing, Heilongjiang 163318, China
2. "Fault Deformation, Sealing and Fluid Migration" Science and Technology Innovation Team in Colleges and Universities of Heilongjiang, Daqing, Heilongjiang 163318, China
3. State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China
4. PetroChina Turpan-Hami Oilfield Company, CNPC, Hami, Xinjiang 839009, China

摘要

摘要: 对三塘湖盆地马朗凹陷主要探井的岩心进行了观察、取样,明确了烃源岩区别于火山岩尤其是凝灰岩的测井响应特征,并通过地质背景与实际井震对比分析,以火山岩与烃源岩的共生关系为依据,通过数学计算模型预测了本区石炭系各主要源岩层系的烃源岩分布。研究结果表明,本区火山岩系共发育两大类烃源岩赋存型式,在火山岩与烃源岩之间存在4种共生关系,测井—地震响应特征明显。石炭系哈尔加乌组和卡拉岗组火山岩与烃源岩的接触关系不同,分属2种不同的火山岩系烃源岩赋存型式,适用于不同的烃源岩厚度数学预测模型。烃源岩分布预测结果表明,卡拉岗组火山岩为陆上喷发,烃源岩空间上与火山岩相隔、独立、正常沉积,分布相对局限;哈尔加乌组火山岩为水下喷发,烃源岩分布广泛但在火山口之间形成多个次级厚度中心,平面分布非均质性较强。
- 烃源岩预测 /
- 测井识别 /
- 地震相 /
- 火山岩系 /
- 马朗凹陷 /
- 三塘湖盆地
Abstract: The formation of volcanic reservoirs in the Malang Sag, the Santanghu Basin is obviously controlled by the distribution of hydrocarbon source rocks. As a result, the identification and prediction of source rocks in the volcanic systems are significant for petroleum exploration. Some core samples have been collected from the study area to calibrate the logging response of source rocks. The distribution of source rocks in different formations of Carboniferous is predicted through mathematical modeling based on the comparison between geologic background and actual logging data, and combined with the symbiotic relationship between source rocks and volcanic rocks. The occurrence of source rocks in the volcanic systems can be categorized into two types, and volcanic rocks coexist with source rocks in four ways, showed by distinctive logging-seismic responses. The contact relationships between source rocks and volcanic rocks in the Haerjiawu and Kalagang formations are quite different, referring to two occurrence types which should be studied with different mathematical models. The Kalagang source rocks are separate and limited in space formed in the normal sedimentation not belonging to the onshore volcanic system. The Haerjiawu source rocks are widespread, forming multiple thickness centers between volcanic vents.
- source rock prediction /
- well logging identification model /
- seismic facies /
- volcanic system /
- Malang Sag /
- Santanghu Basin

HTML全文

参考文献(20)

[1]	顾礼敬,徐守余,苏劲,等.利用地震资料预测和评价烃源岩[J].天然气地球科学, 2011, 22(3):554-560. Gu Lijing,Xu Shouyu,Su Jin,et al.Muddy hydrocarbon source rock prediction and evaluation with seismic data[J].Natural Gas Geoscience,2011,22(3):554-560.
[2]	李松峰,徐思煌,施和生,等.珠江口盆地惠州凹陷古近系烃源岩特征及资源预测[J].地球科学:中国地质大学学报,2013,38(1):112-120. Li Songfeng,Xu Sihuang,Shi Hesheng,et al.Characteristics of Paleogene source rocks and prediction of petroleum resources in Huizhou Depression, Pearl River Mouth Basin[J].Earth Science:Journal of China University of Geosciences,2013,38(1):112-120.
[3]	张波,吴智平,刘华.火成岩在阳信洼陷油气成藏中的地质意义[J].特种油气藏,2014,21(4):80-84. Zhang Bo, Wu Zhiping, Liu Hua.Geological significance of igneous rock to oil/gas reservoir-forming in Yangxin Sag[J].Special Oil & Gas Reservoirs,2014,21(4):80-84.
[4]	Gaibor J,Hochuli J P A,Winkler W,et al.Hydrocarbon source potential of the Santiago Formation,Oriente Basin,SE of Ecuador[J].Journal of South American Earth Sciences,2008,25(2):145-156.
[5]	张文正,杨华,彭平安,等.晚三叠世火山活动对鄂尔多斯盆地长7优质烃源岩发育的影响[J].地球化学,2009,38(6):573-582. Zhang Wenzheng,Yang Hua,Peng Pingan,et al.The influence of late Triassic volcanism on the development of Chang 7 high grade hydrocarbon source rock in Ordos Basin[J].Geochimica,2009,38(6):573-582.
[6]	齐跃春,高红梅,鲍志东,等.漠河盆地依列克得组火山活动间歇期烃源岩有机地球化学特征研究[J].沉积学报,2011,29(1):164-172. Qi Yaochun,Gao Hongmei,Bao Zhidong,et al.Organic geoche-mical characteristics of source rocks from Yiliekede Formation in the intermittent stages of volcanic activity in Mohe Basin[J].Acta Sedimentologica Sinica,2011,29(1):164-172.
[7]	王志宏,罗霞,李景坤,等.松辽盆地北部深层有效烃源岩分布预测[J].天然气地球科学,2008,19(2):204-209. Wang Zhihong,Luo Xia,Li Jingkun,et al.Effective source rock forecasting in deep layers of northern Songliao Basin[J].Natural Gas Geoscience,2008,19(2):204-209.
[8]	何登发,陈新发,况军,等.准噶尔盆地石炭系烃源岩分布与含油气系统[J].石油勘探与开发,2010,37(4):397-408. He Dengfa,Chen Xinfa,Kuang Jun,et al.Distribution of Carbonife-rous source rocks and petroleum systems in the Junggar Basin[J].Petroleum Exploration and Development,2010,37(4):397-408.
[9]	马中远,任丽丹,黄苇,等.塔里木盆地塔中地区火成岩的基本特征[J].特种油气藏,2013,20(3):64-67. Ma Zhongyuan,Ren Lidan,Huang Wei,et al.Basic characteristics of igneous rock in the middle area of Tarim Basin[J].Special Oil & Gas Reservoirs,2013,20(3):64-67.
[10]	Dow W G.Application of oil-correlation and source-rock data to exploration in Williston Basin[J].AAPG Bulletin,1974,58(7):1253-1262.
[11]	管树巍,李本亮,侯连华,等.准噶尔盆地西北缘下盘掩伏构造油气勘探新领域[J].石油勘探与开发,2008,35(1):17-22. Guan Shuwei,Li Benliang,Hou Lianhua,et al.New hydrocarbon exploration areas in footwall covered structures in northwestern margin of Junggar Basin[J].Petroleum Exploration and Deve-lopment,2008,35(1):17-22.
[12]	张义杰,齐雪峰,程显胜,等.准噶尔盆地晚石炭世和二叠纪沉积环境[J].新疆石油地质,2007,28(6):673-675. Zhang Yijie,Qi Xuefeng,Cheng Xiansheng,et al.Approach to sedimentary environment of Late Carboniferous-Permian in Junggar Basin[J].Xinjiang Petroleum Geology,2007,28(6):673-675.
[13]	向奎,鲍志东,庄文山.准噶尔盆地滩坝砂石油地质特征及勘探意义:以排2井沙湾组为例[J].石油勘探与开发,2008,35(2):195-200. Xiang Kui,Bao Zhidong,Zhuang Wenshan.Petroleum geology and exploration of beach sandbar in Junggar Basin,NW China:A case from the Shawan Formation in Well Pai 2[J].Petroleum Exploration and Development,2008,35(2):195-200.
[14]	高岗,梁浩,沈霞,等.三塘湖盆地二叠系火成岩分布及其对烃源岩热演化的影响[J].石油实验地质,2009,32(5):462-465. Gao Gang,Liang Hao,Shen Xia,et al.Permian igneous rock distribution and its influence to the thermal evolution of source rock in Santanghu Basin[J].Petroleum Geology & Experiment,2009,32(5):462-465.
[15]	包建平,马安来,黄光辉,等.三塘湖盆地原油地球化学特征及其成因类型[J].石油勘探与开发,1999,26(4):25-29. Bao Jianping,Ma Anlai,Huang Guanghui,et al.The origin and geochemical characteristics of crude oils from Santanghu basin[J].Petroleum Exploration and Development,1999,26(4):25-29.
[16]	刘俊田.三塘湖盆地牛东地区石炭系卡拉岗组火山岩风化壳模式与识别[J].天然气地球科学,2009,20(1):57-62. Liu Juntian.Weathering crust model and recognition of Carbo-niferous Kalagang Formation (C₂k) volcanic rocks in Niudong Block,Santanghu Basin[J].Natural Gas Geoscience,2009,20(1):57-62.
[17]	Passey Q R,Creaney S,Kulla J B,et al.A practical model for organic richness from porosity and resistivity logs[J].AAPG Bulletin,1990,74(12):1777-1794.
[18]	杨涛涛,范国章,吕福亮,等.烃源岩测井响应特征及识别评价方法[J].天然气地球科学,2013,24(2):414-422. Yang Taotao,Fan Guozhang,Lv Fuliang,et al.The logging features and identification methods of source rock[J].Natural Gas Geoscience,2013,24(2):414-422.
[19]	袁彩萍,徐思煌,薛罗.珠江口盆地惠州凹陷主力烃源岩测井预测及评价[J].石油实验地质,2014,36(1):110-116. Yuan Caiping,Xu Sihuang,Xue Luo.Prediction and evaluation with logging of main source rocks in Huizhou Sag,Pearl River Mouth Basin[J].Petroleum Geology & Experiment,2014,36(1):110-116.
[20]	张文正,杨华,解丽琴,等.湖底热水活动及其对优质烃源岩发育的影响:以鄂尔多斯盆地长₇烃源岩为例[J].石油勘探与开发,2010,37(4):424-429. Zhang Wenzheng,Yang Hua,Xie Liqin,et al.Lake-bottom hydrothermal activities and their influences on the high-quality source rock development:A case from Chang 7 source rocks in Ordos Basin[J].Petroleum Exploration and Development,2010,37(4):424-429.