现代地质
現代地質
현대지질
GEOSCIENCE-JOURNAL OF GRADUATE SCHOOL CHINA UNIVERSITY OF GEOSCIENCES
2013年
5期
999-1004
,共6页
余一欣%周心怀%徐长贵%魏刚%吴奎%张新颖%杨克基
餘一訢%週心懷%徐長貴%魏剛%吳奎%張新穎%楊剋基
여일흔%주심부%서장귀%위강%오규%장신영%양극기
构造变换带%位移守恒%走滑断裂%金县构造%辽东湾坳陷
構造變換帶%位移守恆%走滑斷裂%金縣構造%遼東灣坳陷
구조변환대%위이수항%주활단렬%금현구조%료동만요함
transfer zone%displacement conservation%strike-slip fault%JX structure%Liaodongwan depression
根据地震资料和断层的位移-距离曲线,对辽东湾坳陷中部金县构造变换带的发育特征进行了分析。金县构造是一个发育在走滑断层叠置段内的大型含油气构造,属于郯庐走滑断裂带组成部分的辽中1号断裂带的两条分段断裂在金县地区发生相互作用和叠置,形成了在平面上呈菱形展布的走滑双重构造。菱形断块体同时也传递了分段断层的位移量,使其在空间上保持守恒,从而形成了金县斜向背斜型构造变换带。金县构造变换带的形成演化主要经历了孤立断层发育、变换带初始形成、变换带复杂化和变换带破裂4个阶段。针对渤海地区不同类型构造变换带进行深入分析,对指导油气勘探具有重要意义。
根據地震資料和斷層的位移-距離麯線,對遼東灣坳陷中部金縣構造變換帶的髮育特徵進行瞭分析。金縣構造是一箇髮育在走滑斷層疊置段內的大型含油氣構造,屬于郯廬走滑斷裂帶組成部分的遼中1號斷裂帶的兩條分段斷裂在金縣地區髮生相互作用和疊置,形成瞭在平麵上呈蔆形展佈的走滑雙重構造。蔆形斷塊體同時也傳遞瞭分段斷層的位移量,使其在空間上保持守恆,從而形成瞭金縣斜嚮揹斜型構造變換帶。金縣構造變換帶的形成縯化主要經歷瞭孤立斷層髮育、變換帶初始形成、變換帶複雜化和變換帶破裂4箇階段。針對渤海地區不同類型構造變換帶進行深入分析,對指導油氣勘探具有重要意義。
근거지진자료화단층적위이-거리곡선,대료동만요함중부금현구조변환대적발육특정진행료분석。금현구조시일개발육재주활단층첩치단내적대형함유기구조,속우담려주활단렬대조성부분적료중1호단렬대적량조분단단렬재금현지구발생상호작용화첩치,형성료재평면상정릉형전포적주활쌍중구조。릉형단괴체동시야전체료분단단층적위이량,사기재공간상보지수항,종이형성료금현사향배사형구조변환대。금현구조변환대적형성연화주요경력료고립단층발육、변환대초시형성、변환대복잡화화변환대파렬4개계단。침대발해지구불동류형구조변환대진행심입분석,대지도유기감탐구유중요의의。
Based on seismic data and displacement-distance scaling,this paper analyzes the formation of the JX transfer zone in the middle part of the Liaodongwan depression.The oil-bearing JX structure is a large-scale strike-slip duplex structure where two segmented faults of the Liaozhong-No.1 strike-slip fault overstep and inter-act each other.The rhombic faulted block between the two segmented and overstepped faults transferred their displacements,and the conservation of fault displacements formed the JX transfer zone which belongs to the type of oblique anticline.The JX transfer zone experienced four evolution stages,including the isolated faults,trans-fer zones initiation,complication and rupture.The integrated study on transfer zones has important significance to oil and gas exploration in the offshore part of the Bohai Bay basin.