新疆地质
新疆地質
신강지질
XINJIANG GEOLOGY
2014年
1期
130-135
,共6页
潘力川%王平%庄新国%周继兵%樊涛
潘力川%王平%莊新國%週繼兵%樊濤
반력천%왕평%장신국%주계병%번도
和什托洛盖%层序地层%体系域%聚煤规律
和什託洛蓋%層序地層%體繫域%聚煤規律
화십탁락개%층서지층%체계역%취매규률
Heshituoluogai Basin%Sequence stratigraphy%System tract%Coal accumulation
运用层序地层学有关理论和方法,在钻井资料的基础上,对和什托洛盖盆地下-中侏罗统煤系地层进行了层序地层学与聚煤规律研究。将其下-中侏罗统分为7个三级层序,其中八道湾组、三工河组、西山窑组分别划分出3、2、2个三级层序。通过连井剖面的对比建立了层序地层格架。低位体系域主要发育辫状河、辫状河三角洲、三角洲沉积,湖扩体系域主要发育滨浅湖沉积,高位体系域主要发育三角洲和滨浅湖沉积。煤层主要发育于湖扩期和高位期,相对快的基底沉降和适宜的物源补给对煤的聚集是有利的。
運用層序地層學有關理論和方法,在鑽井資料的基礎上,對和什託洛蓋盆地下-中侏囉統煤繫地層進行瞭層序地層學與聚煤規律研究。將其下-中侏囉統分為7箇三級層序,其中八道灣組、三工河組、西山窯組分彆劃分齣3、2、2箇三級層序。通過連井剖麵的對比建立瞭層序地層格架。低位體繫域主要髮育辮狀河、辮狀河三角洲、三角洲沉積,湖擴體繫域主要髮育濱淺湖沉積,高位體繫域主要髮育三角洲和濱淺湖沉積。煤層主要髮育于湖擴期和高位期,相對快的基底沉降和適宜的物源補給對煤的聚集是有利的。
운용층서지층학유관이론화방법,재찬정자료적기출상,대화십탁락개분지하-중주라통매계지층진행료층서지층학여취매규률연구。장기하-중주라통분위7개삼급층서,기중팔도만조、삼공하조、서산요조분별화분출3、2、2개삼급층서。통과련정부면적대비건립료층서지층격가。저위체계역주요발육변상하、변상하삼각주、삼각주침적,호확체계역주요발육빈천호침적,고위체계역주요발육삼각주화빈천호침적。매층주요발육우호확기화고위기,상대쾌적기저침강화괄의적물원보급대매적취집시유리적。
Based on the principles and methods of the sequence stratigraphy,this study discuss the characteristics of the sequence stratigraphy and coal accumulation of the Jurassic in the Heshituoluogai Basin.3 third-order sequences in Bad-aowan formation,2 third-order sequences in Sangonghe formation,and 2 third-order sequences in Xishanyao formation are distinguished, respectively;Sequence stratigraphical frame was established by contrasting Well profile.The lowstand system tracts are mainly composed of braided river,braided river dalt,dalt sedments;the lake expansion tracts mainly com-posed of shore-shallow lake sedments,the highstand system tracts mainly composed of dalt and shore-shallow lake sed-ments.The coal seams are mainly developed in the lake-expansion and the high-stand system tracts.The relatively quik basin base subside and suitable source of supply is favorable to coal accumulation.