胶州湾的成因及演变
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摘要
胶州湾为一断陷盆地,棋盘格式构造起着主要控制作用。燕山运动晚期奠定了构造格局,全新世海侵形成了今日海湾面貌。该文对盆地形成的火山成因观点提出不同看法,对指导本区域找水、找矿、预防地震等灾害均有重要意义。
Jiaozhou Bay is a fault basin and the chess board structure has played the main control role in its formation. This structural pattern was established in the later period of Yanshanian Movement. It evolved and showed the present features by Holocene transgression. This paper presents a different view from the volcanic cause of formation in the basin formation. And the study is of significance in prospecting water and mine, taking precautions against natural disasters such as earthquakes.
引文
1叶良辅,喻往渊.山东海岸变迁之初步观察及青岛火成岩之研究.国立中央研究院19年度总报告,19302卞云华,汪品先.胶州湾第四纪晚期的微体化石群及其意义.海洋微体古生物论文集.北京:海洋出版社,19803刘洪滨.胶州湾成因.海洋地质与第四纪地质,1986,(3):53~634李善为.从胶州湾沉积物看胶州湾的形成演变.海洋学报,1983,5(3):328~3405青岛科学技术协会.胶州湾综合开发利用.学术讨论会论文汇编,19856尹延鸿,薛春汀.山东崂山劈石口断裂的活动特征.海洋地质与第四纪地质,1987,7(1):123~1267吴桑云等.胶州湾的第四系划分.海洋学报,1995,17(4):78~85

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