石油实验地质
石油實驗地質
석유실험지질
EXPERIMENTAL PETROLEUM GEOLOGY
2013年
3期
296-301
,共6页
周长迁%张庆春%杨沛广%段海岗
週長遷%張慶春%楊沛廣%段海崗
주장천%장경춘%양패엄%단해강
主控因素%成藏模式%美索不达米亚盆地%伊拉克
主控因素%成藏模式%美索不達米亞盆地%伊拉剋
주공인소%성장모식%미색불체미아분지%이랍극
main controlling factor%accumulation model%Mesopotamia Basin%Iraq
美索不达米亚盆地是全球油气最富集的盆地之一,主要产层为白垩系.在构造、沉积、钻井、测试等资料基础之上,研究认为多套优质成熟烃源岩、有利的储盖组合、一系列大型背斜圈闭控制着盆地内大型油气田的形成.受成藏条件控制,盆地中—南部和北部发育2种不同的成藏模式.盆地中—南部发育下生上储型的生储盖组合,油气以通过输导层的水平运移为主,烃源岩差异造成原油性质的差异.盆地北部,侏罗系—下白垩统烃源岩生成的油气沿大型走滑断层运移到上白垩统储层,油气的差异运移聚集作用造成油气藏原油特征下轻上重.
美索不達米亞盆地是全毬油氣最富集的盆地之一,主要產層為白堊繫.在構造、沉積、鑽井、測試等資料基礎之上,研究認為多套優質成熟烴源巖、有利的儲蓋組閤、一繫列大型揹斜圈閉控製著盆地內大型油氣田的形成.受成藏條件控製,盆地中—南部和北部髮育2種不同的成藏模式.盆地中—南部髮育下生上儲型的生儲蓋組閤,油氣以通過輸導層的水平運移為主,烴源巖差異造成原油性質的差異.盆地北部,侏囉繫—下白堊統烴源巖生成的油氣沿大型走滑斷層運移到上白堊統儲層,油氣的差異運移聚集作用造成油氣藏原油特徵下輕上重.
미색불체미아분지시전구유기최부집적분지지일,주요산층위백성계.재구조、침적、찬정、측시등자료기출지상,연구인위다투우질성숙경원암、유리적저개조합、일계렬대형배사권폐공제착분지내대형유기전적형성.수성장조건공제,분지중—남부화북부발육2충불동적성장모식.분지중—남부발육하생상저형적생저개조합,유기이통과수도층적수평운이위주,경원암차이조성원유성질적차이.분지북부,주라계—하백성통경원암생성적유기연대형주활단층운이도상백성통저층,유기적차이운이취집작용조성유기장원유특정하경상중.
@@@@The Mesopotamia Basin is one of the most prolific petroliferous basins in the world. The most impor-tant productive layer is Cretaceous. Based on the comprehensive analyses of structure, sedimentary, drilling and testing, the paper summarizes the controlling factors of hydrocarbon accumulation. They are high-quality source rocks, good reservoir-seal assemblages, huge structural traps, migration pathways and so on. There are two kinds of accumulation models in the Mesopotamia Basin. In the center and south of the basin, petroleum gene-rates in the lower formation and is reserved in the upper formation. Carrier beds are the main pathways for oil-and-gas migrations in the parallel direction. The characteristics of petroleum are controlled by source rocks. In the north, oil and gas migrate from the Jurassic and the Lower Cretaceous source rocks to the Upper Cretaceous reservoirs along strike slip faults. The differential hydrocarbon accumulations lead to light oil in the lower forma-tion and heavy oil in the upper formation.