闽东滨海断裂带活动特征研究
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摘要
地质构造是影响人类生存发展的重要因素。断层是岩层或岩体顺破裂而发生明显位移的构造。断层在地壳中广泛发育，是地壳中最重要的构造之一。断层常常构成一定地区的构造格架。一些区域性巨型断层不仅控制或影响区域地质构造的结构和发展，而且常常控制和影响区域成矿作用，并以其为背景形成区域成矿带。一些中小型断层直接决定了某些矿体的形态和产状，对石油、天然气、地下水等矿藏的分布、储聚和运移也有重要影响，尤其是现代活动性断层更直接影响水工建筑和工程活动，所以断层的研究不论在理论上还是实践上均具有十分重要的意义。
本文根据2006年在福建近海开展的多道地震的勘探成果，结合该区历史沉积资料，探讨闽东滨海海底断裂构造的分布特征，通过对地震采集资料的解译，推断其新近活动时期为中新世晚期～上新世初期，并以遥感卫片为辅助手段，分析沿岸线性构造与滨海断裂之间的关系。航天遥感技术和卫片的采用，扩大了观察地质构造的视域和深度，弥补了野外地质观察的局限性，而物探、钻孔等工程和探测技术在本文中则为了解海底断层结构、规模提供了重要佐证，判断该断裂已达大断裂的规模。
Geological structure is an important factor that influences the survival and development of humankind. Fault is obvious displacement structure caused by fracture of rock formation or rock mass. Fault becomes one of the most important crustal structures as it develops extensively in terrestrial crust. In some areas, fault is their tectonic framework for most of the time. Part of the regional mega faults control and influence not only geological structure and its development in some regions but also its mineralization, which sets as background to form regional metallogenetic belt. Some minor faults directly determine the structure and the occurrence of certain ore body, having great effect on the distribution, reservation and migration of some mineral resources such as petroleum, natural gas and underground water. Faults, especially modern active faults can even influence marine engineering construction. Therefore, the investigation into fault is of great significance in both theory and practice.
Based on several seismic prospecting results in offshore Fujian province in 2006, combining with historical sediment data collected in this area, this paper aims at discussing the distribution characteristics of submarine offset structure in East Fujian coast area. It can be inferred that the recent active period in this area would be during late Miocene and early Pliocene. Moreover, assisted with remote sensoring satellite photos, this paper tries to analyze the relationship between costal linear structure and offshore fracture. By using space remote sensoring technology and satellite photos, people can widen the observation and deepen the understanding of geological structure, which makes up for the limitness of field geological observation. Besides7 the application of geophysical exploration and drilling technology supplies important proof for Understanding submarine offset structure and scale in this survey. It comes to the conclusion. that the fracture has spread in large scale.
本文根据2006年在福建近海开展的多道地震的勘探成果，结合该区历史沉积资料，探讨闽东滨海海底断裂构造的分布特征，通过对地震采集资料的解译，推断其新近活动时期为中新世晚期～上新世初期，并以遥感卫片为辅助手段，分析沿岸线性构造与滨海断裂之间的关系。航天遥感技术和卫片的采用，扩大了观察地质构造的视域和深度，弥补了野外地质观察的局限性，而物探、钻孔等工程和探测技术在本文中则为了解海底断层结构、规模提供了重要佐证，判断该断裂已达大断裂的规模。
Geological structure is an important factor that influences the survival and development of humankind. Fault is obvious displacement structure caused by fracture of rock formation or rock mass. Fault becomes one of the most important crustal structures as it develops extensively in terrestrial crust. In some areas, fault is their tectonic framework for most of the time. Part of the regional mega faults control and influence not only geological structure and its development in some regions but also its mineralization, which sets as background to form regional metallogenetic belt. Some minor faults directly determine the structure and the occurrence of certain ore body, having great effect on the distribution, reservation and migration of some mineral resources such as petroleum, natural gas and underground water. Faults, especially modern active faults can even influence marine engineering construction. Therefore, the investigation into fault is of great significance in both theory and practice.
Based on several seismic prospecting results in offshore Fujian province in 2006, combining with historical sediment data collected in this area, this paper aims at discussing the distribution characteristics of submarine offset structure in East Fujian coast area. It can be inferred that the recent active period in this area would be during late Miocene and early Pliocene. Moreover, assisted with remote sensoring satellite photos, this paper tries to analyze the relationship between costal linear structure and offshore fracture. By using space remote sensoring technology and satellite photos, people can widen the observation and deepen the understanding of geological structure, which makes up for the limitness of field geological observation. Besides7 the application of geophysical exploration and drilling technology supplies important proof for Understanding submarine offset structure and scale in this survey. It comes to the conclusion. that the fracture has spread in large scale.
引文
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[6] 吴时国，刘展，王万银等．东沙群岛海区晚新生代构造特征及其对弧-陆碰撞的响应．海洋与湖沼．2004，35(6)：481-490．
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[11] 杨木壮，王明君，梁金强等。南海万安盆地构造沉降及其油气成藏控制作用．海洋地质与第四纪地质，2003，23(2)：85-88．
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[13] Sloss L.L.. Integrated facies analysis . Geol. Soc. Am. Bull ,1949, pp91-124.
[14] Sloss L.L.. Forty years of sequence stratigraphy. Geol. Soc. Am. Bull, 1988, pp1661-1682.
[15] Vail P R, Mitchum R M, Jr Todd R B, Widmier J M et al.. Seismic stratigraphy and global changes of sea level[J]. In: Clayton C E ed., Seismic Stratigraphy-Applications to Hydrocarbon Eploration, Am. Assoc. Petroleum Geologists Mem., 1977, 26: 49～212.
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[17] Van Wagoner J C, Mitchum R M, Campion K M et al.. Siliciclastic sequence stratigraphy in Well Logs, Cores and outcrops: Concepts for High-Resolutions Correlation of Time and Facies[J]. AAPG Methods in Exploration Series, 1990, 7:1～57.
[18] 丁志俊主编．城市地震小区划及工程地震勘探．北京：地震出版社，1991．
[19] 刘保全．浅层地震勘探在岩溶调查中的应用效果．物探与化探，1996，20(6)：474-475．
[20] 贝智敏，邬庆良，王允洪。地震方法在平湖油气田发现和早期开发中的应用[A]。刘申叔、李上卿．东海油气地球物理勘探．北京：地质出版社 2001，212-219．
[21] 贾健谊，顾惠荣．东海西湖凹陷含油气系统与油气资源评价．北京：地质出版社，2002，19-29．
[22] 黄慈流等，台湾海峡西部地质、地球物理和地球化学综合调查研究。厦门：厦门大学出版社，1997，28-50．
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