新疆石油地质
新疆石油地質
신강석유지질
XINJIANG PETROLEUM GEOLOGY
2010年
2期
211-215
,共5页
丁增勇%陈文学%熊丽萍%林卫东%许华明%田纳新
丁增勇%陳文學%熊麗萍%林衛東%許華明%田納新
정증용%진문학%웅려평%림위동%허화명%전납신
奥连特盆地%不整合%类型%结构%油气运移%油气聚集
奧連特盆地%不整閤%類型%結構%油氣運移%油氣聚集
오련특분지%불정합%류형%결구%유기운이%유기취집
Oriente basin%unconformity%type%structure%petroleum migration%petroleum accumulation
拉美地区在世界油气资源中所处地位不断提高,奥连特盆地属于该地区勘探与开发程度较高的重要含油气盆地.为加深对奥连特盆地构造演化及其控藏规律的认识,将奥连特盆地构造演化史大体划分为古生代被动陆缘、中生代弧后裂谷及新生代弧后前陆3个阶段.根据断裂发育及沉降一沉积特征,将奥连特盆地划分为西部次安第斯构造带、中部构造带及东部前陆斜坡构造带3个构造单元.构造演化对该盆地油气成藏具有控制作用,中部构造带西(早)安第斯阶段多形成低幅背斜圈闭,西部、东部构造带东(晚)安第斯阶段分别以形成逆冲断背斜型圈闭和构造一岩性复合型圈闭为主.
拉美地區在世界油氣資源中所處地位不斷提高,奧連特盆地屬于該地區勘探與開髮程度較高的重要含油氣盆地.為加深對奧連特盆地構造縯化及其控藏規律的認識,將奧連特盆地構造縯化史大體劃分為古生代被動陸緣、中生代弧後裂穀及新生代弧後前陸3箇階段.根據斷裂髮育及沉降一沉積特徵,將奧連特盆地劃分為西部次安第斯構造帶、中部構造帶及東部前陸斜坡構造帶3箇構造單元.構造縯化對該盆地油氣成藏具有控製作用,中部構造帶西(早)安第斯階段多形成低幅揹斜圈閉,西部、東部構造帶東(晚)安第斯階段分彆以形成逆遲斷揹斜型圈閉和構造一巖性複閤型圈閉為主.
랍미지구재세계유기자원중소처지위불단제고,오련특분지속우해지구감탐여개발정도교고적중요함유기분지.위가심대오련특분지구조연화급기공장규률적인식,장오련특분지구조연화사대체화분위고생대피동륙연、중생대호후렬곡급신생대호후전륙3개계단.근거단렬발육급침강일침적특정,장오련특분지화분위서부차안제사구조대、중부구조대급동부전륙사파구조대3개구조단원.구조연화대해분지유기성장구유공제작용,중부구조대서(조)안제사계단다형성저폭배사권폐,서부、동부구조대동(만)안제사계단분별이형성역충단배사형권폐화구조일암성복합형권폐위주.
Oriente basin is one of the important petroliferous basins of Latin American region with higher levels of exploration and development. For the purpose of in-depth understanding of the tectonic evolution and the oil accumulation controhnent in Oriente basin, the study of the sedimentary strata distribution and tectonic subsidence has been carried out through the overall consideration of MOP (Mranon-Oriente-Putumayo) petroleum province consisting of Ecuador's Oriente basin, Colombia's Putumaro basin and Peru's Maranon basin. Based on subsidence mechanism and sedimentary strata, Oriente basin is roughly divided into three stages in tectonic evolution, i.e. Paleozoic passive continental margin, Mesozoic back-arc rift and Cenozoic back-arc foreland. According to the characteristics of faults, considering subsidence-sedimentation characteristics of the entire MOP petroleum province, Oriente basin could be spatially divided into three tectonic units, i.e. the western sub-Andean belt, the central belt and the eastern foreland slope belt. Tectonic evolution has an absolutely dominant role in controlling hydrocarbon accumulation. Lots of low-amplitude anticline traps were formed mostly during the west (early) Andes episode in the central tectonic belt. Principal traps belong to reverse-thrust anticline traps and composite traps of structure-lithology formed during the east (late) Andes episode respectively in the western and eastern tectonic belts.