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作 者:孟祥君[1,2] 张训华[1,2] 杨金玉[1,2]
机构地区:[1]国土资源部海洋油气资源和环境地质重点实验室,青岛266071 [2]青岛海洋地质研究所,青岛266071
出 处:《海洋地质与第四纪地质》2014年第6期127-134,共8页Marine Geology & Quaternary Geology
基 金:国家重点基础研究发展计划项目(2013CB429701);中国地质调查项目(GZH201400205);国家自然科学基金国际合作交流项目(41210005);国家自然科学基金青年基金项目(41206050)
摘 要:中国海洋地质调查始于20世纪50年代,大致分为创业阶段、起步阶段、发展阶段、全面发展阶段和蓬勃发展阶段,经过多年的地质与地球物理调查,获取了大量的地质地球物理资料。该区磁场强度一般为±200nT,局部达到±500nT以上,呈NE、NNE向作带状分布,局部异常走向不一,类型多变。空间和布格重力异常总体走向为NE向,陆区以负异常为主,海区主要表现为正异常,空间重力异常值总体上为-45^+100mGal,局部异常值可达+200mGal以上;布格重力异常极小值为-140mGal,极大值可达+440mGal,局部地区分布高值异常圈闭。根据重、磁异常的幅值高低、形态展布和区域变化等特征,将重、磁异常各自划分为华北-渤海异常区、山东半岛-北黄海异常区等9个异常区,重磁场特征充分展示了中国东部海区东西分带、南北分块的构造格局。Marine geophysical investigation in China started from 50's of the last century.It could be roughly divided into the starting-up stage,early stage,developing stage,rapid developing stage and accelerated developing stage.A large number of high-resolution geological and geophysical data have been acquired by the surveys in the past years.With regard to the magnetic data,the background of magnetic anomalies is± 200 nT,with some anomalies higher than±500nT occurring in some local areas.Most of the anomalies extend in NE or NNE direction in a band pattern.However,some anomalies vary in both types and distribution patterns.Free air and Bouguer gravity anomalies are also showing a NE distribution pattern.In a general view,negative anomalies prevail in land,whereas the sea is dominated by positive anomalies.The intensity of free air gravity anomalies normally vary in the range of-45and+100mGal,with some of anomalies higher than+200mGal in local areas.The intensity of Bouguer gravity anomalies change between-140 and +440mGal.According to the intensity of gravity and magnetic anomalies,in combination with the characteristics of geomorphology,we may divide the region into nine areas,such as the North China-Bohai magnetic anomaly area and Shandong peninsula-north Yellow Sea anomaly area.The distribution pattern of"zoning in east-west direction and blocking in north-south direction"is rather obvious.
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