赤水及邻区燕山期古构造特征与油气聚集关系
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摘要
中国石油化工股份有限公司南方勘探开发分公司研究院,云南昆明650200为了弄清赤水及邻区燕山期古构造特征与油气聚集的关系,首先应用钻井资料、地震资料、部分野外露头实测资料,以陆相碎屑岩地层的5个界面为研究对象,采用"标志层"拉平技术——标志层一厚度法恢复了主要目的层在燕山期的古构造面貌,查清了古隆起的分布范围,编制了古构造图,并分析了古构造的发育情况和演化特征。须家河底面的古构造总体上表现为"三隆两凹"的构造格局;须家河顶面的古构造主要表现为被"X"形的古凹陷分割的4个古隆起平台;东岳庙顶面和凉高山顶面的古构造相似,具有继承性发育的特点。大致以现今的官渡构造带为界,工区东部古构造形态相对较简单,凸起和凹陷的幅度均不大,中西部古构造相对较发育,表现为多凸多凹.凸凹相间的古构造格局。结合前人对区内生烃史和烃源岩演化史的研究结果,分析了古构造与油气聚集的关系.认为燕山期古隆起与下伏海相烃源岩和上三叠统烃源岩的生烃高峰期相匹配,是油气运聚的有利指向区。
The study focuses on the relationship between paleostructure characteristics and hydrocarbon accumulation in ChiShui and neigh- boring area during Yanshan stage.Firstly,taking the five inter- faces of continental clastic formation as target,we use the‘marker bed’flattening technology,drilling data,seismic data and part of field crop actual data to restore the palaeostructure of intended in- tervals in Yanshan stage,identify the distribution of paleohigh, draw the palaeostructure map,and analyze the development and e- volution features of palaeostructure.The palaeostructure at the bottom of Xujiahe displays‘three uplifts and two depressions’di- vided by X-shaped paleo-depression into four paleohigh platforms. The paleostructures on the top of Dongyuemiao and Liaogao Moun- tain are similar in the feature of successional development with the Guandu structure belt being its boundary.The paleostructure shape in eastern working area is relatively simple and both the re- lief of uplifts and the depressions are small in scale.The paleo- structure in the middle and the west is relatively well developed, showing a paleostrueture pattern of numerous and alternative up- lifts and depressions.Then,combined with the former research re- sults of hydrocarbon-generation history and hydrocarbon source rock evolution history in this area,the relationship of paleostruc- ture and hydrocarbon accumulation is analyzed,indicating that the paleohigh of Yanshan stage well matches the hydrocarbon-genera- ted fastigium of underlying marine and Upper Triassic hydrocarbon source rock and so is the beneficial zone of hydrocarbon migration and accumulation.
The study focuses on the relationship between paleostructure characteristics and hydrocarbon accumulation in ChiShui and neigh- boring area during Yanshan stage.Firstly,taking the five inter- faces of continental clastic formation as target,we use the‘marker bed’flattening technology,drilling data,seismic data and part of field crop actual data to restore the palaeostructure of intended in- tervals in Yanshan stage,identify the distribution of paleohigh, draw the palaeostructure map,and analyze the development and e- volution features of palaeostructure.The palaeostructure at the bottom of Xujiahe displays‘three uplifts and two depressions’di- vided by X-shaped paleo-depression into four paleohigh platforms. The paleostructures on the top of Dongyuemiao and Liaogao Moun- tain are similar in the feature of successional development with the Guandu structure belt being its boundary.The paleostructure shape in eastern working area is relatively simple and both the re- lief of uplifts and the depressions are small in scale.The paleo- structure in the middle and the west is relatively well developed, showing a paleostrueture pattern of numerous and alternative up- lifts and depressions.Then,combined with the former research re- sults of hydrocarbon-generation history and hydrocarbon source rock evolution history in this area,the relationship of paleostruc- ture and hydrocarbon accumulation is analyzed,indicating that the paleohigh of Yanshan stage well matches the hydrocarbon-genera- ted fastigium of underlying marine and Upper Triassic hydrocarbon source rock and so is the beneficial zone of hydrocarbon migration and accumulation.
引文
1胡东风．赤水地区阳新灰岩储层勘探分析[J]．云南地质，1999，18(3)：326～333
2王良军，胡东风．赤水及邻区须家河组成藏主控因素及有利区带分析[J]．南方油气，2005，18(1)：9～12
3陈立官．油气田地下地质学[M]．北京：地质出版社，1984．133～137
4王香文，于常青，董宁等．储层综合预测技术在鄂尔多斯盆地定北区块的应用[J]．石油物探，2006，45(3)：267～271
5田晶莹．鬲寿和．应用VSP资料进行地震特征波组的地质层位标定[J]．石油物探，2000，39(4)：100～106
6安作相．泸州古隆起与川南油气[J]．石油实验地质，1996，18(3)：267～273
7安作相．泸州古隆起及嘉陵江灰岩含油气性的三个问题[J]．西安石油学院学报，1997，12(2)：16～20
8胡光灿，谢姚祥．中国四川东部高陡构造石炭系气田[M]．北京：石油工业出版社，1997．119～134
9李晓清，汪泽成，张兴为等．四川盆地古隆起特征及对天然气的控制作用[J]．石油与天然气地质，2001，22 (4)：347～351
10刘特民．贵州赤水及邻区裂缝性气藏模式探讨[J]．海相油气地质，1996，1(4)：40～44
2王良军，胡东风．赤水及邻区须家河组成藏主控因素及有利区带分析[J]．南方油气，2005，18(1)：9～12
3陈立官．油气田地下地质学[M]．北京：地质出版社，1984．133～137
4王香文，于常青，董宁等．储层综合预测技术在鄂尔多斯盆地定北区块的应用[J]．石油物探，2006，45(3)：267～271
5田晶莹．鬲寿和．应用VSP资料进行地震特征波组的地质层位标定[J]．石油物探，2000，39(4)：100～106
6安作相．泸州古隆起与川南油气[J]．石油实验地质，1996，18(3)：267～273
7安作相．泸州古隆起及嘉陵江灰岩含油气性的三个问题[J]．西安石油学院学报，1997，12(2)：16～20
8胡光灿，谢姚祥．中国四川东部高陡构造石炭系气田[M]．北京：石油工业出版社，1997．119～134
9李晓清，汪泽成，张兴为等．四川盆地古隆起特征及对天然气的控制作用[J]．石油与天然气地质，2001，22 (4)：347～351
10刘特民．贵州赤水及邻区裂缝性气藏模式探讨[J]．海相油气地质，1996，1(4)：40～44
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