准噶尔盆地车莫古隆起侏罗系剥蚀厚度恢复
|
摘要
车莫古隆起位于准噶尔盆地腹部,为一个南西—北东走向的燕山期古隆起,现今构造为由北向南倾斜的单斜。该区侏罗纪经历了多期构造运动,发育多个削蚀和上超不整合面,是地层岩性油气藏勘探的有利地区。通过地层剥蚀厚度恢复主要方法与相关条件的分析,根据研究区实际地震资料特征,采用地震剖面直接追踪法、参考层厚度变化率法和邻层厚度比值法,对车莫古隆起区侏罗系头屯河组、西山窑组、三工河组的剥蚀厚度进行了恢复,其最大剥蚀量均分布在奎屯—莫索湾一带,各层最大剥蚀厚度为260m、340m和140m。其中古隆起高部位的西山窑组剥蚀量可能是由两期构造运动造成的,三工河组剥蚀量的产生可能来自后期构造运动。通过分析剥蚀厚度平面分布特征与古隆起形成、演化之间的关系,指出早侏罗世末期是车莫古隆起的雏形期,西山窑组沉积期是车莫古隆起的逐渐发育时期,侏罗纪末期是车莫古隆起快速发育时期。大量剥蚀产物的搬运为古隆起翼部斜坡区地层岩性圈闭的形成创造了条件,车莫古隆起南部斜坡区是油气聚集的有利地区。
The Chemo palaeouplift is located in the interior of the Junggar Basin. It is oriented in SW-NE direction which was formed in the Yanshanian Orogeny. Now it is a monocline with a north to south inclination. The Jurassic of the study area experienced a multi-stage tectonic movements. Many truncations and onlap unconformity surfaces were developed, thus the study area is profitable for exploration of lithologic petroleum accumulations. By analyses on the eroded stratigraphic thickness and according to the seismic profiles characters, the eroded thickness of the Toutunhe, the Xishanyao and the Sangonghe formations of the Jurassic in the Chemo palaeouplift are reconstructed using the direct seismic profile indexing method combined with the thickness viriation ratio method and the neighboring thickness ratio method. The most intensive erosion occurred in the Kuitun-Mosuowan area, and the largest eroded thickness is 260 m, 340 m, and 140 m respectively for the three formations. The eroded thickness of the Xishanyao Formation in the high palaeouplift was probably formed by two-stage tectonic movements, while the eroded thickness of the Sangonghe Formation in the higher palaeouplift was probably from the tectonic movement in the later period. The relationship between the planar distribution characters of the eroded thickness and the formation and evolution of the palaeouplift indicate the late Early Jurassic is the initial forming period of the Chemo palaeouplift, the sedimentary period of Xishanyao Formation is its developing period, and the Late Jurassic is its extensively developing period. The transportation of a great deal of eroded sediment provided the conditions for the lithologic trap formation on the slope area of the palaeouplift. The southern slope area of the Chemo palaeouplift is the profitable petroleum accumulation area.
The Chemo palaeouplift is located in the interior of the Junggar Basin. It is oriented in SW-NE direction which was formed in the Yanshanian Orogeny. Now it is a monocline with a north to south inclination. The Jurassic of the study area experienced a multi-stage tectonic movements. Many truncations and onlap unconformity surfaces were developed, thus the study area is profitable for exploration of lithologic petroleum accumulations. By analyses on the eroded stratigraphic thickness and according to the seismic profiles characters, the eroded thickness of the Toutunhe, the Xishanyao and the Sangonghe formations of the Jurassic in the Chemo palaeouplift are reconstructed using the direct seismic profile indexing method combined with the thickness viriation ratio method and the neighboring thickness ratio method. The most intensive erosion occurred in the Kuitun-Mosuowan area, and the largest eroded thickness is 260 m, 340 m, and 140 m respectively for the three formations. The eroded thickness of the Xishanyao Formation in the high palaeouplift was probably formed by two-stage tectonic movements, while the eroded thickness of the Sangonghe Formation in the higher palaeouplift was probably from the tectonic movement in the later period. The relationship between the planar distribution characters of the eroded thickness and the formation and evolution of the palaeouplift indicate the late Early Jurassic is the initial forming period of the Chemo palaeouplift, the sedimentary period of Xishanyao Formation is its developing period, and the Late Jurassic is its extensively developing period. The transportation of a great deal of eroded sediment provided the conditions for the lithologic trap formation on the slope area of the palaeouplift. The southern slope area of the Chemo palaeouplift is the profitable petroleum accumulation area.
引文
陈中红,查明,朱筱敏.2003.准噶尔盆地陆梁隆起不整合面与油气运聚关系[J].古地理学报,5(1):120-126.
咚殿君,任建业,任亚平.2006.准噶尔盆地车莫古隆起的演化及其对油气藏的控制[J].油气地质与采收率,13(3):39-42.
何登发,翟光明,况军,等.2005.准噶尔盆地古隆起的分布与基本特征[J].地质科学,40(2):248-261.
匡立春,吕焕通,齐雪峰,等.2005.准噶尔盆地岩性油气藏勘探成果和方向[J].石油勘探与开发,32(6):32-37.
刘小平,杨立干,徐健,等.2004.苏北盆地高邮凹陷始新统剥蚀厚度恢复[J].新疆石油地质,25(2):128-130.
刘学锋,何幼斌,张或丹.1999.利用回剥分析重建古构造格局——以川、鄂、湘边区为例[J].古地理学报,1(2):53-61.
牟中海,唐勇,崔炳富,等.2002.塔西南地区地层剥蚀厚度恢复研究[J].石油学报,23(1):40-44.
谭开俊,牟中海.2004.塔西南地区上寒武统—奥陶系剥蚀厚度恢复[J].河南石油,18(3):4-6.
佟彦明,宋立军,曾少军,等.2005.利用镜质体反射率恢复地层剥蚀厚度的新方法[J].古地理学报,7(3):417-424.
佟彦明,吴冲龙.2006.Ro差值法恢复地层剥蚀量的不合理性[J].天然气工业,26(5):21-23.
吴晓智,张年富,石昕,等.2006.准噶尔盆地车莫古隆起构造特征与成藏模式[J].中国石油勘探,11(1):65-68.
张满郎,张琴,朱筱敏,等.2000.准噶尔盆地阜东斜坡区侏罗系层序地层学研究[J].古地理学报,2(3):27-36.
真柄钦次著,陈荷立等译.1981.压实与流体运移[M].北京:石油工业出版社,8-30.
周路,张义杰,雷德文,等.2005.准噶尔盆地莫索湾凸起构造特征[J].中国石油勘探,10(1):16-21.
Chen Zhonghong,Zha Ming,Zhu Xiaomin.2003.Relation between un-conformity surface and hydrocarbon migration and accumulation ofLuliang uplift in Junggar Basin[J].Journal of Palaeogeography,5(1):120-126(in Chinese with English abstract).
Dong Dianjun,Ren Jianye,Ren Yaping.2006.Evolution of the ChemoPalaeouplift in Junggar Basin and control on the oil and gas reservoir[J].Oil&Gas Recovery Technology,13(3):39-42(in Chinesewith English abstract).
He Dengfa,Zhai Guangming,Kuang Jun,et al.2005.Distribution andtectonic features of Paleouplifts in the Junggar Basin[J].ChineseJournal of Geology,40(2):248-261(in Chinese with English ab-stract).
Kuang Lichun,Lu Huantong,Qi Xuefeng,et al.2005.Exploration andtargets for lithologic reservoirs in Junggar Basin[J].Petroleum Ex-ploration and Development,32(6):32-37(in Chinese with Eng-lish abstract).
Liu Xiaoping,Yang Ligan,Xu Jian,et al.2004.Restoration of Eoceneerosion thickness in Gaoyou Sag[J].Xinjiang Petroleum Geology,25(2):128-130(in Chinese with English abstract).
Liu Xuefeng,He Youbin,Zhang Huodan.1999.Palaeotectonic recon-struction using backstripping analysis:Example from the border are-as of Sichuan,Hubei and Hunan Provinces[J].Journal of Palaeo-geography,1(2):53-61(in Chinese with English abstract).
Magara K(ed),Chen Heli,et al.(translators).1981.Compaction and Fluid Migration[M].Beijing:Petroleum Industry Press,8-30(in Chinese).
Mu Zhonghai,Tang Yong,Cui Bingfu,et al.2002.Erosion thicknessrestoration in Southwest Tarim Basin[J].Acta Petrolei Sinica,23(1):40-44(in Chinese with English abstract).
Tan Kaijun,Mu Zhonghai.2004.Restoration of erosion thickness of Up-per Cambrian Ordovician in Southwest Area of Tarim Basin[J].Henan Petroleum,18(3):4-6(in Chinese with English abstract).
Tong Yanming,Song Lijun,Zeng Shaojun,et al.2005.A new methodby vitrinite reflectance to estimate thickness of eroded strata[J].Journal of Palaeogeography,7(3):417-424(in Chinese with Eng-lish abstract).
Tong Yanming,Wu Chonglong.2006.Irrationality of calculating denu-dation thickness of strata withRo-difference method[J].NaturalGas Industry,26(5):21-23(in Chinese with English abstract).
Wu Xiaozhi,Zhang Nianfu,Shi Xin,et al.2006.Characteristics andreservoiring mode of Chepaizi-Mosuowan Palaeouplift in Junggar Ba-sin[J].China Petroleum Exploration,11(1):65-68(in Chinesewith English abstract).
Zhang Manlang,Zhang Qin,Zhu Xiaomin,et al.2000.Sequence Stra-tigraphy of Jurassic on the East Fukang Slope,Junggar Basin[J].Journal of Palaeogeography,2(3):27-36(in Chinese with Englishabstract).
Zhou Lu,Zhang Yijie,Lei Dewen,et al.2005.Structural characters ofMosuowan Uplift in Junggar Basin[J].China Petroleum Explora-tion,10(1):16-21(in Chinese with English abstract).
咚殿君,任建业,任亚平.2006.准噶尔盆地车莫古隆起的演化及其对油气藏的控制[J].油气地质与采收率,13(3):39-42.
何登发,翟光明,况军,等.2005.准噶尔盆地古隆起的分布与基本特征[J].地质科学,40(2):248-261.
匡立春,吕焕通,齐雪峰,等.2005.准噶尔盆地岩性油气藏勘探成果和方向[J].石油勘探与开发,32(6):32-37.
刘小平,杨立干,徐健,等.2004.苏北盆地高邮凹陷始新统剥蚀厚度恢复[J].新疆石油地质,25(2):128-130.
刘学锋,何幼斌,张或丹.1999.利用回剥分析重建古构造格局——以川、鄂、湘边区为例[J].古地理学报,1(2):53-61.
牟中海,唐勇,崔炳富,等.2002.塔西南地区地层剥蚀厚度恢复研究[J].石油学报,23(1):40-44.
谭开俊,牟中海.2004.塔西南地区上寒武统—奥陶系剥蚀厚度恢复[J].河南石油,18(3):4-6.
佟彦明,宋立军,曾少军,等.2005.利用镜质体反射率恢复地层剥蚀厚度的新方法[J].古地理学报,7(3):417-424.
佟彦明,吴冲龙.2006.Ro差值法恢复地层剥蚀量的不合理性[J].天然气工业,26(5):21-23.
吴晓智,张年富,石昕,等.2006.准噶尔盆地车莫古隆起构造特征与成藏模式[J].中国石油勘探,11(1):65-68.
张满郎,张琴,朱筱敏,等.2000.准噶尔盆地阜东斜坡区侏罗系层序地层学研究[J].古地理学报,2(3):27-36.
真柄钦次著,陈荷立等译.1981.压实与流体运移[M].北京:石油工业出版社,8-30.
周路,张义杰,雷德文,等.2005.准噶尔盆地莫索湾凸起构造特征[J].中国石油勘探,10(1):16-21.
Chen Zhonghong,Zha Ming,Zhu Xiaomin.2003.Relation between un-conformity surface and hydrocarbon migration and accumulation ofLuliang uplift in Junggar Basin[J].Journal of Palaeogeography,5(1):120-126(in Chinese with English abstract).
Dong Dianjun,Ren Jianye,Ren Yaping.2006.Evolution of the ChemoPalaeouplift in Junggar Basin and control on the oil and gas reservoir[J].Oil&Gas Recovery Technology,13(3):39-42(in Chinesewith English abstract).
He Dengfa,Zhai Guangming,Kuang Jun,et al.2005.Distribution andtectonic features of Paleouplifts in the Junggar Basin[J].ChineseJournal of Geology,40(2):248-261(in Chinese with English ab-stract).
Kuang Lichun,Lu Huantong,Qi Xuefeng,et al.2005.Exploration andtargets for lithologic reservoirs in Junggar Basin[J].Petroleum Ex-ploration and Development,32(6):32-37(in Chinese with Eng-lish abstract).
Liu Xiaoping,Yang Ligan,Xu Jian,et al.2004.Restoration of Eoceneerosion thickness in Gaoyou Sag[J].Xinjiang Petroleum Geology,25(2):128-130(in Chinese with English abstract).
Liu Xuefeng,He Youbin,Zhang Huodan.1999.Palaeotectonic recon-struction using backstripping analysis:Example from the border are-as of Sichuan,Hubei and Hunan Provinces[J].Journal of Palaeo-geography,1(2):53-61(in Chinese with English abstract).
Magara K(ed),Chen Heli,et al.(translators).1981.Compaction and Fluid Migration[M].Beijing:Petroleum Industry Press,8-30(in Chinese).
Mu Zhonghai,Tang Yong,Cui Bingfu,et al.2002.Erosion thicknessrestoration in Southwest Tarim Basin[J].Acta Petrolei Sinica,23(1):40-44(in Chinese with English abstract).
Tan Kaijun,Mu Zhonghai.2004.Restoration of erosion thickness of Up-per Cambrian Ordovician in Southwest Area of Tarim Basin[J].Henan Petroleum,18(3):4-6(in Chinese with English abstract).
Tong Yanming,Song Lijun,Zeng Shaojun,et al.2005.A new methodby vitrinite reflectance to estimate thickness of eroded strata[J].Journal of Palaeogeography,7(3):417-424(in Chinese with Eng-lish abstract).
Tong Yanming,Wu Chonglong.2006.Irrationality of calculating denu-dation thickness of strata withRo-difference method[J].NaturalGas Industry,26(5):21-23(in Chinese with English abstract).
Wu Xiaozhi,Zhang Nianfu,Shi Xin,et al.2006.Characteristics andreservoiring mode of Chepaizi-Mosuowan Palaeouplift in Junggar Ba-sin[J].China Petroleum Exploration,11(1):65-68(in Chinesewith English abstract).
Zhang Manlang,Zhang Qin,Zhu Xiaomin,et al.2000.Sequence Stra-tigraphy of Jurassic on the East Fukang Slope,Junggar Basin[J].Journal of Palaeogeography,2(3):27-36(in Chinese with Englishabstract).
Zhou Lu,Zhang Yijie,Lei Dewen,et al.2005.Structural characters ofMosuowan Uplift in Junggar Basin[J].China Petroleum Explora-tion,10(1):16-21(in Chinese with English abstract).
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心