地质科学
地質科學
지질과학
SCIENTIA GEOLOGICA SINICA
2010年
1期
243-255
,共13页
谭佳奕%王淑芳%张元元%吴润江%郭召杰
譚佳奕%王淑芳%張元元%吳潤江%郭召傑
담가혁%왕숙방%장원원%오윤강%곽소걸
火山岩特征%火山机构%早石炭世%巴塔玛依内山组%准噶尔盆地东部
火山巖特徵%火山機構%早石炭世%巴塔瑪依內山組%準噶爾盆地東部
화산암특정%화산궤구%조석탄세%파탑마의내산조%준갈이분지동부
Volcanics characteristics%Volcanic edifice%Early Carboniferous%Batamayinieshan Formation%Eastern Junggar Basin
准噶尔盆地东部石炭系火山岩油气藏勘探近年来取得了重大成就.该区石炭系巴塔玛依内山组火山岩储层类型多样,包括玄武岩、安山岩和流纹岩等火山熔岩,火山集块、火山角砾岩、凝灰岩等火山碎屑岩以及各种沉积一火山岩.火山岩存在多期次、间歇性喷发的特征,一般至少可以划分为3个喷发期次,沉积岩夹层是其主要喷发间断面,两个沉积夹层之间的火山岩层段是有利储集段带.该区石炭纪古火山机构类型多样.近火山通道火山角砾岩发育,是有利的储集相带.综合古生物化石证据和同位素年代学资料,火山活动时限为早石炭世,该区石炭系地层自下而上应为下石炭统塔木岗组、滴水泉组和巴塔玛依内山组;上石炭统为石钱滩组.
準噶爾盆地東部石炭繫火山巖油氣藏勘探近年來取得瞭重大成就.該區石炭繫巴塔瑪依內山組火山巖儲層類型多樣,包括玄武巖、安山巖和流紋巖等火山鎔巖,火山集塊、火山角礫巖、凝灰巖等火山碎屑巖以及各種沉積一火山巖.火山巖存在多期次、間歇性噴髮的特徵,一般至少可以劃分為3箇噴髮期次,沉積巖夾層是其主要噴髮間斷麵,兩箇沉積夾層之間的火山巖層段是有利儲集段帶.該區石炭紀古火山機構類型多樣.近火山通道火山角礫巖髮育,是有利的儲集相帶.綜閤古生物化石證據和同位素年代學資料,火山活動時限為早石炭世,該區石炭繫地層自下而上應為下石炭統塔木崗組、滴水泉組和巴塔瑪依內山組;上石炭統為石錢灘組.
준갈이분지동부석탄계화산암유기장감탐근년래취득료중대성취.해구석탄계파탑마의내산조화산암저층류형다양,포괄현무암、안산암화류문암등화산용암,화산집괴、화산각력암、응회암등화산쇄설암이급각충침적일화산암.화산암존재다기차、간헐성분발적특정,일반지소가이화분위3개분발기차,침적암협층시기주요분발간단면,량개침적협층지간적화산암층단시유리저집단대.해구석탄기고화산궤구류형다양.근화산통도화산각력암발육,시유리적저집상대.종합고생물화석증거화동위소년대학자료,화산활동시한위조석탄세,해구석탄계지층자하이상응위하석탄통탑목강조、적수천조화파탑마의내산조;상석탄통위석전탄조.
Exploration on oil-gas reservoir of the Carboniferous volcanic rocks made great successes in recent years. In this area,the types of volcanic reservoir of Batamayineishan Formation are diverse,including lavas,such as basalt,andesite,rhyolitea et al.,pyroclastics,as volcanic agglomerate,breccias tuff and different sedimentary-volcanic rocks.The volcanic rocks characterize multiple stages and intermittent eruption.The complete cross section of Batamayineishan Formiaton are grouped at least three stages,with sedimentary interbeds as discontinuity surface.The volcanic rocks are favorable reservoirs between two interbeds.The types of ancient volcanic edifices are various.The regions nearby volcanic conduit,riched in pyroclastics,are advantage zones for reservoirs.Combined data of isotopic chronology and fossil evidence,it is certain that the time of volcano eruption is early Carboniferous.The stratas of Cauboniferous in the study area from below is Tamugang,Dishuiquan and Batamayineishan Formation of lower Carboniferous and Shiqiantan Formation of upper Carboniferous.