STUDY ON STRATA EROSION THICKNESS RESTORATION IN NORTHEAST DEPRESSION OF SOUTH YELLOW SEA BASIN
-
摘要: 地层抬升剥蚀是沉积盆地中普遍存在的现象。地层剥蚀厚度的准确恢复对正确重建沉积盆地原始沉积-构造演化史,热史及油气生、排、运、聚史和定量评价油气资源潜力至关重要。本次研究在充分结合南黄海北部盆地东北凹陷区域构造和演化特征研究的基础之上,依据东北凹陷实际地质情况和资料条件,选取参考层厚度变化率法和沉积速率法,对东北凹陷始新统戴南组和三垛组地层的剥蚀厚度进行了定量恢复。结果表明,渐新世末的三垛运动使东北凹陷内始新统戴南组和三垛组地层遭受强烈的剥蚀改造,戴南组和三垛组地层在凹陷内各个构造带表现出不同的剥蚀响应特征。Abstract: The uplift and erosion of strata are ubiquitous in sedimentary basins. Restoring exact thickness of the erosion is very important to rebuild rationally the histories of initial deposition-tectonic evolution, geothermal, hydrocarbon generation, expulsion, migration and accumulation, and also to evaluate accurately the potential of oil and natural gas resources.On the basis of researches on tectonic evolution in northeast depression of the South Yellow Sea basin and according to practical geological conditions and present information, the method for thickness variance ratio of reference layer and sedimentation rate was applied to the eroded thickness restoration of Eocene Dainan formation and Sanduo formation in northeast depression. The final result suggested that the Sanduo tectonic movement which occurred at the last stage of Eocene, resulted in the intense erosion of Eocene Dainan formation and Sanduo formation,and these two formations indicate distinct characteristics in different tectonic zones of the northeast depression.
-
Keywords:
- eroded strata thickness /
- Eocene /
- northeast depression /
- South Yellow Sea basin
-
-
[1] 陈颐亨.浅析南黄海的找油气前景[J]. 海洋地质与第四纪地质,1984,4(2):49-55. [CHEN Yiheng. A preliminary analysis of hydrocarbon potential of the South Yellow Sea[J]. Marine Geology and Quaternary Geology, 1984,4(2):49-55.]
[2] 蔡乾忠.黄海含油气盆地区域地质与大地构造环境[J].海洋地质动态,2002,18(11):8-12. [CAI Qianzhong. Regional geology and geotectonic environment of petroliferous basins in the Yellow Sea[J]. Marine Geology Letters, 2002,18(11):8-12.]
[3] 王胜利,卢华复,李刚,等. 南黄海盆地北部凹陷古近纪伸展断层转折褶皱作用[J]. 石油与天然气地质,2006,27(4):495-503. [WANG Shengli, LU Huafu, LI Gang, et al.Paleogene extensional fault-bend folding in north depression of southern Yellow Sea Basin[J]. Oil and Gas Geology, 2006,27(4):495-503.]
[4] 牟中海,唐勇,崔炳富,等.塔西南地区地层剥蚀厚度恢复研究[J].石油学报,2002,23(1):40-44. [MOU Zhonghai, TANG Yong, CUI Bingfu, et al. Erosion thickness restoration in southwest Tarim Basin[J]. Acta Petrolei Sinica,2002,23(1):40-44.]
[5] 何生,王青玲. 关于用镜质体反射率恢复地层剥蚀厚度的问题讨论[J]. 地质论评,1989, 35(2):119-125. [HE Sheng, WANG Qingling. The eroded thickness reconstructed by vitrinite reflectance[J]. Geological Review, 1989, 35(2):119-125.]
[6] 胡圣标.利用镜质体反射率数据估算地层剥蚀厚度[J].石油勘探与开发,1999,26(4):42-45. [HU Shengbiao. Estimation of the amount of erosion thickness using vitrinite reflectance data.[J].Petroleum Exploration and Development, 1999,26(4):42-45.]
[7] 陈增智,柳广弟,郝石生. 修正的镜质体反射率剥蚀厚度恢复方法[J].沉积学报,1999,17(1):141-144. [CHEN Zengzhi, LIU Guangdi, HAO Shisheng. A corrected method using vitrinite reflectance data to estimate the thickness of sediment removed at unconformity[J].Acta Sedimentologica Sinica,1999,17(1):141-144.]
[8] Magara K. Thickness of removed sedimentary rocks, paleoporepressure, and paleotemperature,southwestern part of Western Canada basin[J].AAPG Bulletin, 1976,60:554-566.
[9] 真柄钦次,陈荷立译. 压实与流体运移[M].北京:石油工业出版社,1981:8-30.[Magara K,CHEN Heli. Geochemistry of Oilfield Waters[M].Beijing:Petroleum Industry Press,1981:8 -30.]
[10] 马立祥. 利用砂岩孔隙度演化趋势估计古地层剥蚀量的简易方法[J]. 石油实验地质,1991,13(1):53-55. [MA Lixiang.Simplified method to estimate denudation amount in palaeostrata with the evolutionary trend of porosity in sandstone[J].Petroleum Geology and Experiment,1991,13(1):53-55.]
[11] 刘景彦,林畅松,喻岳钰,等.用声波测井资料计算剥蚀量的方法改进[J].石油实验地质,2000,22(4):302-306. [LIU Jingyan, LIN Changsong, YU Yueyu, et al. An improved method to calculate denuded amount by sonic well logs[J].Petroleum Geology and Experiment, 2000,22(4):302-306.]
[12] 吴智平,刘继国,张卫海,等.辽河盆地东部凹陷北部地区新老第三纪界面地层剥蚀量研究[J]. 高校地质学报, 2001,37(1):99-106. [WU Zhiping, LIU Jiguo, ZHANG Weihai, et al. Study on the erosion amount of hiatus surface between Neogene and Eogene in north part of east depression, Liaohe Basin[J].Geological Journal of China University, 2001,37(1):99-106.]
[13] 何将启,周祖翼,江兴歌,等. 优化孔隙度法计算地层剥蚀厚度:原理及实例[J]. 石油实验地质, 2002,24(6):561-565. [HE Jiangqi,ZHOU Zuyi, JIANG Xingge,et al.Optimum estimation of the amount of erosion by porosity data:the theory and example[J].Experiment and Petroleum Geology, 2002,24(6):561-565.]
[14] 王震,张明利,王子煜,等.东海陆架盆地西湖凹陷不整合面剥蚀厚度恢复[J] 石油实验地质, 2005,27(1):90-93. [WANG Zhen, ZHANG Mingli, WANG Ziyu, et al. Erosion thickness restoration of unconformities in the Xihu Sag, the shelf basin of East China Sea[J].Experiment and Petroleum Geology, 2005,27(1):90-93.]
[15] 刘国臣,金之钧,李京昌. 沉积盆地沉积-剥蚀过程定量研究的一种新方法——盆地波动分析应用之一[J]. 沉积学报, 1995,13(3):23-31 [LIU Guochen, JING Zhijun, LI Jingchang. A new method on the quantitative study of depositional and erosional processes of sedimentary basins-An application of wave process analysis during basin evolution[J].Acta Sedimentologica Sinica,1995,13(3):23-31.]
[16] Dow W G. Kerogen studies and geological interpretations[J].Journal of Geochemical Exploration, 1977, 7:79-99.
[17] Katz B J, Phelfer R N, Schunk D J. Interpretation of discontinuous vitrinite reflectance profiles[J]. AAPG Bulletin, 1988,72(8):926-931.
[18] Lastett G M, Green P F, Duddy I R, et al. Thermal annealing of fission tracks in apatite:A quantitative analysis[J]. Chemical Geology,1987, 73(25):25-38.
[19] 周礼成,冯石,王世成. 用裂变径迹长度分布模拟地层剥蚀量和热史[J].石油学报,1994, 15(3):26-37. [ZHOU Licheng, FENG Shi, WANG Shicheng. Strata erosion amount and geothermal history modeling by analysis of apatite fission track length distribution[J].Acta Sedimentologica Sinica, 1994,15(3):26-37.]
[20] Guidish T M, Kendall C G, Lerche I, et al. Basin evaluation using burial history calculations:an overview[J]. AAPG Bulletin, 1985, 69(1):92-105.
[21] 李伟.恢复地层剥蚀厚度方法综述[J].中国海上油气(地质),1996,10(3):167-171.[LI Wei. Summary of reconstruction of strata denudation thickness[J].China Offshore Oil and Gas, 1996,10(3):167-171.] [22] 王毅,金之钧.沉积盆地中恢复地层剥蚀量的新方法[J].地球科学进展,1999,14(5):482-486 [WANG Yi, JIN Zhijun.Progress of the methods on the recovery of the thickness of eroded strata in basin[J].Advance in Earth Sciences, 1999,14(5):482-486.]
[23] 谭开俊,牟中海. 塔西南地区上寒武统-奥陶系剥蚀厚度恢复[J]. 河南石油,2004,18(3):4-7. [TAN Kaijun, MOU Zhonghai. Restoration of erosion thickness of upper Cambrian-Ordovician in southwest area of Tarim Basin[J]. Henan Petroleum,2004,18(3):4-7.]
计量
- 文章访问数: 2200
- HTML全文浏览量: 228
- PDF下载量: 19