东海陆架盆地南部及邻区陆域中生界对比
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摘要
为了探讨东海陆架盆地南部中生界油气勘探前景,在对现有的钻井资料、地震剖面和重磁资料处理的基础上,对东海陆架盆地南部及邻区陆域的中生界岩相组合和地层展布特征进行分析对比。综合研究认为:陆域中生界分布广,但发育不均,沉积类型多样,火山活动频繁;海域中生界分布广、厚度大,呈现"东厚西薄、南厚北薄"的特征。海陆中生界的差异主要表现在:陆域中生界受火山活动影响较大,以陆相火山岩沉积为主,而海域中生界受火山活动影响相对较小,主要为受海侵影响的湖相沉积。因此,由陆到海,中生界岩性变细、颜色变暗,海域的生烃潜力可能优于陆域。
In order to further understand the distribution pattern of the Mesozoic strata in the southern East China Sea Shelf Basin,this paper deals with the lithofacies assemblages and stratigraphic distribution in the southern East China Sea Shelf Basin and its adjacent areas,upon the geological and geophysical data recently acquired from seismic survey,drilling,gravity-magnetic survey and field observations.The results suggest that the Mesozoic strata in the adjacent areas of the basin are widely distributed and characterized by heterogeneous sedimentary sequences and strong volcanic activities,whereas the Mesozoic strata in the basin cover an extensive area with a large thickness over 6000m,which is thick in the south and east,but thin in the north and west'.There are obvious differences between the land and the sea:the land is more affected by volcanic activities and dominated by continental volcanic deposits,while the sea area is less affected by volcanic activities and dominated by lacustrine deposits under the influence of marine transgression.The sediments become finer and darker in the basin.Therefore,the sea area is more favorable for hydrocarbon exploration.
In order to further understand the distribution pattern of the Mesozoic strata in the southern East China Sea Shelf Basin,this paper deals with the lithofacies assemblages and stratigraphic distribution in the southern East China Sea Shelf Basin and its adjacent areas,upon the geological and geophysical data recently acquired from seismic survey,drilling,gravity-magnetic survey and field observations.The results suggest that the Mesozoic strata in the adjacent areas of the basin are widely distributed and characterized by heterogeneous sedimentary sequences and strong volcanic activities,whereas the Mesozoic strata in the basin cover an extensive area with a large thickness over 6000m,which is thick in the south and east,but thin in the north and west'.There are obvious differences between the land and the sea:the land is more affected by volcanic activities and dominated by continental volcanic deposits,while the sea area is less affected by volcanic activities and dominated by lacustrine deposits under the influence of marine transgression.The sediments become finer and darker in the basin.Therefore,the sea area is more favorable for hydrocarbon exploration.
引文
[1]赖万忠.中国海域中生界油气勘探[J].中国海上油气(地质),2001,15(5):311-316.
[2]高乐.东海陆架中生代残留盆地特征及勘探方向探讨[J].中国海上油气,2005,17(3):148-152.
[3]徐立明,邓克,卢清地,等.东海陆架盆地南部邻近陆域中生代盆地演化研究[R].福建:福建省地质调查研究院,2012.
[4]冯晓杰,蔡东升,王春修,等.东海陆架盆地中新生代构造演化特征[J].中国海上油气(地质),2003,17(1):33-37.
[5]周蒂.台西南盆地和北港隆起的中生界及其沉积环境[J].热带海洋学报,2002,21(2):50-57.
[6]须雪豪,陈琳琳,汪企浩.东海陆架盆地中生界地质特征与油气资源潜力浅析[J].海洋石油,2004,24(3):1-7.
[7]梁建设,王存武,郭瑞,等.东海陆架盆地南部新生界油气资源潜力评价[R].北京:中海石油(中国)有限公司,2012.
[8]王可德,王建平,徐国庆,等.东海陆架盆地西南部中生代地层的发现[J].地层学杂志,2000,24(2):129-131.
[9]龚建明,李刚,杨传胜,等.东海陆架盆地南部中生界分布特征与油气勘探前景[J].吉林大学学报(地球科学版),2013,24(1):11-16.
[2]高乐.东海陆架中生代残留盆地特征及勘探方向探讨[J].中国海上油气,2005,17(3):148-152.
[3]徐立明,邓克,卢清地,等.东海陆架盆地南部邻近陆域中生代盆地演化研究[R].福建:福建省地质调查研究院,2012.
[4]冯晓杰,蔡东升,王春修,等.东海陆架盆地中新生代构造演化特征[J].中国海上油气(地质),2003,17(1):33-37.
[5]周蒂.台西南盆地和北港隆起的中生界及其沉积环境[J].热带海洋学报,2002,21(2):50-57.
[6]须雪豪,陈琳琳,汪企浩.东海陆架盆地中生界地质特征与油气资源潜力浅析[J].海洋石油,2004,24(3):1-7.
[7]梁建设,王存武,郭瑞,等.东海陆架盆地南部新生界油气资源潜力评价[R].北京:中海石油(中国)有限公司,2012.
[8]王可德,王建平,徐国庆,等.东海陆架盆地西南部中生代地层的发现[J].地层学杂志,2000,24(2):129-131.
[9]龚建明,李刚,杨传胜,等.东海陆架盆地南部中生界分布特征与油气勘探前景[J].吉林大学学报(地球科学版),2013,24(1):11-16.
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