-
摘要:
根据2014—2017年在霞浦近岸海域实测得的约3 500 km浅地层剖面和同网布设的单道地震剖面、侧扫声纳等地球物理资料,结合遥感影像和岸滩监测剖面等数据,综合运用海洋沉积学、层序地层学、构造地质学等方法,识别了研究区内存在的主要潜在海洋灾害地质因素,包括埋藏古河道、浅层气、浅埋不规则基岩面、楔形泥质体、潮流沙脊、海岸线变迁等,简要分析了其特征、成因机制和危害性,为探讨研究区的灾害地质防治奠定理论基础,为海洋资源开发及海洋工程建设提供科学依据。
Abstract:About 3500km of geophysical data were collected from the coastal area of Xiapu, Fujian province during the period from 2014 to 2017, which include measured shallow seismic stratigraphic profiles, single-channel seismic sections and side-scan sonars as well as remote sensing images and coastal monitoring profiles. Incorporated with the careful study of marine sedimentology, sequence stratigraphy and structural geology, various marine geo-hazards are discovered, such as buried paleo- channels, shallow gas accumulations, shallow buried irregular bedrocks, muddy areas, tidal sand ridges, and abandoned coasts. We described and discussed the characteristics and genetic mechanism of these potential hazards in this paper in order to lay a foundation for further exploring geo-hazard factors in the study area so as to provide a scientific basis for marine resource development and marine engineering construction in the coastal areas along northern Fujian.
-
Key words:
- geohazard factor /
- shallow gas /
- paleo-channel /
- coastal area of northern Fujian
-
-
表 1 闽北近岸海域潜在灾害地质因素分类
Table 1. Classification of potential marine geo-hazards in North of Fujian coastal area
存在位置 潜在灾害地质因素 海底表层 楔形泥质体、水下浅滩、海岸线变迁 海底埋藏 埋藏古河道、浅层气、浅埋不规则基岩面、埋藏沙脊 -
[1] 李恒鹏, 杨桂山.长江三角洲与苏北海岸动态类型划分及侵蚀危险度研究[J].自然灾害学报, 2001, 10(4):20-25. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zrzhxb200104004
[2] 刘守全, 刘锡清, 王圣洁, 等.南海灾害地质类型及分区[J].中国地质灾害与防治学报, 2000, 11(4):39-44. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdzzhyfzxb200004009
[3] 李西双, 刘保华, 郑彦鹏, 等.黄东海灾害地质类型及声学反射特征[J].中国海洋大学学报:自然科学版, 2002, 32(1):107-114. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=qdhydxxb200201014
[4] 仇建东, 刘健, 孔祥淮, 等.山东半岛南部滨浅海区的海洋灾害地质[J].海洋地质与第四纪地质, 2012, 32(1):27-33. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201201005
[5] Liu J P, Li A C, Xu K H, et al. Sedimentary features of the Yangtze River-derived along-shelf clinoform deposit in the East China Sea[J]. Continental Shelf Research, 2006, 26(17):2141-2156. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cb0de1e2c1f888760bbc88e5eb37620e
[6] 刘升发, 石学法, 刘焱光, 等.东海内陆架泥质区沉积速率[J].海洋地质与第四纪地质, 2009, 29(6):5-11. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz200906001
[7] 石学法, 刘升发, 乔淑卿, 等.东海闽浙沿岸泥质区沉积特征与古环境记录[J].海洋地质与第四纪地质, 2010, 30(4):19-30. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201004004
[8] 孔祥淮, 刘健, 杜远生, 等.南黄海西部滨浅海区灾害地质因素特征及分布规律[J].海洋地质与第四纪地质, 2012, 32(2):43-52. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201202005
[9] 吕炳全.海洋地质学概论[M].上海:同济大学出版社, 2008.
[10] 叶银灿, 陈俊仁, 潘国富, 等.海底浅层气的成因、赋存特征及其对工程的危害[J].海洋学研究, 2003, 21(1):28-37. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dhhy200301005
[11] 顾兆峰, 张志珣, 刘怀山.南黄海西部地区浅层气地震特征[J].海洋地质与第四纪地质, 2006, 26(3):65-74. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz200603010
[12] 王雅丽, 王明田, Wang Y L, 等.浅层气探测及其海洋工程响应[J].中国造船, 2005, 46(b11):120-125. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgzc2005z1019
[13] 李萍, 杜军, 刘乐军, 等.我国近海海底浅层气分布特征[J].中国地质灾害与防治学报, 2010, 21(1):69-74. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdzzhyfzxb201001015
[14] 詹文欢, 孙宗勋, 朱俊江, 等.珠江口海岛及海域地质环境与灾害初探[J].海洋地质与第四纪地质, 2001, 21(4):31-36. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz200104006
[15] 吴自银, 曹振轶, 王小波, 等.海底沙脊地貌的研究现状及进展[J].海洋学研究, 2006, 24(3):53-63. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dhhy200603006
[16] Taylor D I.Nearshore shallow gas around the UK coast[J].Continental Shelf Research, 1992, 12:1135-1144. doi: 10.1016/0278-4343(92)90074-T
-