海相油气地质
海相油氣地質
해상유기지질
MARINE ORIGIN PETROLEUM GEOLOGY
2014年
2期
15-22
,共8页
沙旭光%马庆佑%吕海涛%李晓益%朱秀香
沙旭光%馬慶祐%呂海濤%李曉益%硃秀香
사욱광%마경우%려해도%리효익%주수향
塔里木盆地%古城墟隆起%奥陶系%油气成藏%油源对比%地球化学特征%主控因素
塔裏木盆地%古城墟隆起%奧陶繫%油氣成藏%油源對比%地毬化學特徵%主控因素
탑리목분지%고성허륭기%오도계%유기성장%유원대비%지구화학특정%주공인소
Ordovician%Hydrocarbon accumulation%Oil-source correlation%Geochemical characteristics%Guchengxu Uplift%Tarim Basin
古城墟隆起奥陶系海相碳酸盐岩地层近年来相继发现了一些出油气井,已经成为塔里木盆地的重点勘探目标区。目前已证实古城墟隆起存在奥陶系一间房组顶部灰岩与鹰山组内幕灰质白云岩两套含油气层系。奥陶系主要为正常压力、高温的干气气藏,但顺南1井一间房组顶部的原油属低硫、低蜡轻质油,表现出典型的凝析油特征。综合油气性质、生物标志化合物特征及烃包裹体发育特征,认为该区主要存在两期油气充注过程:第一期油气充注发生在加里东晚期-海西早期,以来自寒武系-下奥陶统烃源岩的原油为主;第二期油气充注发生在喜马拉雅期,以寒武系过成熟的干气为主,气侵改造导致该区以纯气藏和凝析气藏为主。古城墟隆起已钻井均见到不同级别的油气显示,并且不含水,初步研究认为优质的碳酸盐岩储层是油气成藏的最关键因素,同时北东向断裂对油气成藏有重要影响。
古城墟隆起奧陶繫海相碳痠鹽巖地層近年來相繼髮現瞭一些齣油氣井,已經成為塔裏木盆地的重點勘探目標區。目前已證實古城墟隆起存在奧陶繫一間房組頂部灰巖與鷹山組內幕灰質白雲巖兩套含油氣層繫。奧陶繫主要為正常壓力、高溫的榦氣氣藏,但順南1井一間房組頂部的原油屬低硫、低蠟輕質油,錶現齣典型的凝析油特徵。綜閤油氣性質、生物標誌化閤物特徵及烴包裹體髮育特徵,認為該區主要存在兩期油氣充註過程:第一期油氣充註髮生在加裏東晚期-海西早期,以來自寒武繫-下奧陶統烴源巖的原油為主;第二期油氣充註髮生在喜馬拉雅期,以寒武繫過成熟的榦氣為主,氣侵改造導緻該區以純氣藏和凝析氣藏為主。古城墟隆起已鑽井均見到不同級彆的油氣顯示,併且不含水,初步研究認為優質的碳痠鹽巖儲層是油氣成藏的最關鍵因素,同時北東嚮斷裂對油氣成藏有重要影響。
고성허륭기오도계해상탄산염암지층근년래상계발현료일사출유기정,이경성위탑리목분지적중점감탐목표구。목전이증실고성허륭기존재오도계일간방조정부회암여응산조내막회질백운암량투함유기층계。오도계주요위정상압력、고온적간기기장,단순남1정일간방조정부적원유속저류、저사경질유,표현출전형적응석유특정。종합유기성질、생물표지화합물특정급경포과체발육특정,인위해구주요존재량기유기충주과정:제일기유기충주발생재가리동만기-해서조기,이래자한무계-하오도통경원암적원유위주;제이기유기충주발생재희마랍아기,이한무계과성숙적간기위주,기침개조도치해구이순기장화응석기장위주。고성허륭기이찬정균견도불동급별적유기현시,병차불함수,초보연구인위우질적탄산염암저층시유기성장적최관건인소,동시북동향단렬대유기성장유중요영향。
Guchengxu Uplift in which commercial oil and gas have been drilled out in Ordovician marine carbonate rocks in some wells in recent years has become one of the exploration focus areas in Tarim basin. Two series of Ordovician hydrocarbon-bearing reservoirs have b een confirmed to be present in Guchengxu Uplift, one is the limestone at the top of Ordovician Yijianfang Formation and the other is the limy dolostone of internal Ordovician Yingshan Formation. The hydrocarbon is present mostly in dry-gas state with normal pressure and high temperature in Ordovician reservoirs but exceptionally, light oil with low content of sulfur and wax which is characteristic of condensate oil are drilled out in the top of Yijianfang Formation in Well SN-1. Combined with the analysis of hydrocarbon property, biomarkers and hydrocarbon inclusion characteristics, it is suggested that two periods of hydrocarbon emplacement experienced in this uplift. Emplacing oil derived from the Cambrian to lower Ordovician source rocks in the first period of emplacement that occurred during the late Caledonian to Early Hercynian movements, and emplacing over-mature dry gas were dominated in the second period of emplacement that occurred during Himalayan movement. The following gas emplacement resulted in forming pure gas or condensate gas reservoirs. Different ranks of oil/gas shows are present in the drilled wells in Guchengxu Uplift, and specially all of oil and gas yielded are with no water. It is generally considered that high-quality carbonate reservoirs are the key for hydrocarbon accumulation and the developing NE-trending faults play an important role in hydrocarbon accumulation.