大地构造与成矿学
大地構造與成礦學
대지구조여성광학
Geotectonica et Metallogenia
2015年
5期
795-807
,共13页
谢玉洪%童传新%范彩伟%宋鹏%张昊%童亨茂
謝玉洪%童傳新%範綵偉%宋鵬%張昊%童亨茂
사옥홍%동전신%범채위%송붕%장호%동형무
琼东南盆地%断裂系统%先存构造%构造样式%两期伸展
瓊東南盆地%斷裂繫統%先存構造%構造樣式%兩期伸展
경동남분지%단렬계통%선존구조%구조양식%량기신전
Qiongdongnan Basin%fault system%pre-existing weakness%structural style%two-phase extension
在对二、三维地震资料系统解释的基础上,通过不同区域断层分布特征和演化及盆地结构的差异性分析,将琼东南盆地北部坳陷带划分为两个断裂系统(东部断裂系统和西部断裂系统)及8个子系统,并阐述分析了各子断裂系统的断层分布特征和规律。再利用平衡剖面技术,研究分析了琼东南盆地断裂系统的演化阶段和断层的活动期次,确定“长期活动型”、“早衰型”、“中期活动型”(分“中期活动Ⅰ型”和“中期活动Ⅱ型”)、“晚成型”等4个系列的断层占主导地位。分析确定琼东南盆地复杂的断裂系统是在先存构造条件下,两期不同方向伸展变形叠加而成,其中南北向伸展的递进变形起主导作用;不同区域先存构造分布和活动的差异是造成琼东南盆地断裂系统复杂性的根本原因。
在對二、三維地震資料繫統解釋的基礎上,通過不同區域斷層分佈特徵和縯化及盆地結構的差異性分析,將瓊東南盆地北部坳陷帶劃分為兩箇斷裂繫統(東部斷裂繫統和西部斷裂繫統)及8箇子繫統,併闡述分析瞭各子斷裂繫統的斷層分佈特徵和規律。再利用平衡剖麵技術,研究分析瞭瓊東南盆地斷裂繫統的縯化階段和斷層的活動期次,確定“長期活動型”、“早衰型”、“中期活動型”(分“中期活動Ⅰ型”和“中期活動Ⅱ型”)、“晚成型”等4箇繫列的斷層佔主導地位。分析確定瓊東南盆地複雜的斷裂繫統是在先存構造條件下,兩期不同方嚮伸展變形疊加而成,其中南北嚮伸展的遞進變形起主導作用;不同區域先存構造分佈和活動的差異是造成瓊東南盆地斷裂繫統複雜性的根本原因。
재대이、삼유지진자료계통해석적기출상,통과불동구역단층분포특정화연화급분지결구적차이성분석,장경동남분지북부요함대화분위량개단렬계통(동부단렬계통화서부단렬계통)급8개자계통,병천술분석료각자단렬계통적단층분포특정화규률。재이용평형부면기술,연구분석료경동남분지단렬계통적연화계단화단층적활동기차,학정“장기활동형”、“조쇠형”、“중기활동형”(분“중기활동Ⅰ형”화“중기활동Ⅱ형”)、“만성형”등4개계렬적단층점주도지위。분석학정경동남분지복잡적단렬계통시재선존구조조건하,량기불동방향신전변형첩가이성,기중남북향신전적체진변형기주도작용;불동구역선존구조분포화활동적차이시조성경동남분지단렬계통복잡성적근본원인。
On the basis of systematic structural interpretation of the 2D and 3D seismic data and analysis of the fault distribution and evolution, and basin structure in different regions, the Northern Depression Zone of the Qiongdongnan Basin is divided into two fault systems (Eastern and Western fault systems) and eight sub-fault systems. The characteristics and patterns of fault distribution in each sub-fault system are described in this paper. The evolution stages of the fault systems and their activation phases were also analyzed with balanced section technology. Four dominant evolution patterns of the faults, including“long-term activity type”,“premature type”,“mid-term activity type”(further subdivided into“mid-term activity type Ⅰ”and“mid-term activity type Ⅱ”), and“late activity type”, were recognized. We concluded that the complicated fault systems in the Qiongdongnan Basin were formed by the superposition of two phases of extension with different extension direction, while the NS direction extension played a primary role. The difference of pre-existing weakness distribution and activation in different regions is primary cause for the complexity of the fault systems in the Qiongdongnan Basin.