新疆地质
新疆地質
신강지질
XINJIANG GEOLOGY
2014年
2期
255-260
,共6页
阿力木江·吐斯依提%庄新国%潘立川%李宝庆
阿力木江·吐斯依提%莊新國%潘立川%李寶慶
아력목강·토사의제%장신국%반립천%리보경
库拜煤田%塔里奇克组%层序%聚煤规律
庫拜煤田%塔裏奇剋組%層序%聚煤規律
고배매전%탑리기극조%층서%취매규률
Kuqa-Bay Coalfield%Taliqike Formation%Sequence Strata%Coal accumulation
探讨了库拜煤田下侏罗统塔里奇克组的聚煤特征与聚煤规律。据基础资料,采用层序地层、沉积体系等分析方法,建立塔里奇克组等时地层格架,分析层序格架下煤层发育及分布规律,总结塔里奇克组聚煤的层序地层学模式,预测煤炭资源时空分布。认为塔里奇克组可划分出两个三级层序,分别为SQ1、SQ2;煤层主要分布于SQ1、SQ2的湖扩和高位体系域;SQ1、SQ2中湖扩、高位体系域均有较连续煤层发育,湖扩体系域煤层好于高位体系域的。
探討瞭庫拜煤田下侏囉統塔裏奇剋組的聚煤特徵與聚煤規律。據基礎資料,採用層序地層、沉積體繫等分析方法,建立塔裏奇剋組等時地層格架,分析層序格架下煤層髮育及分佈規律,總結塔裏奇剋組聚煤的層序地層學模式,預測煤炭資源時空分佈。認為塔裏奇剋組可劃分齣兩箇三級層序,分彆為SQ1、SQ2;煤層主要分佈于SQ1、SQ2的湖擴和高位體繫域;SQ1、SQ2中湖擴、高位體繫域均有較連續煤層髮育,湖擴體繫域煤層好于高位體繫域的。
탐토료고배매전하주라통탑리기극조적취매특정여취매규률。거기출자료,채용층서지층、침적체계등분석방법,건립탑리기극조등시지층격가,분석층서격가하매층발육급분포규률,총결탑리기극조취매적층서지층학모식,예측매탄자원시공분포。인위탑리기극조가화분출량개삼급층서,분별위SQ1、SQ2;매층주요분포우SQ1、SQ2적호확화고위체계역;SQ1、SQ2중호확、고위체계역균유교련속매층발육,호확체계역매층호우고위체계역적。
This paper aims to investigate coal accumulation under the sequence strata from Taliqike formation of Kuqa-Bay Coalfield. Based on existing data, and combined with analysis methods of sequence stratigraphy and depositional systems, this paper established isochronous stratigraphic framework of Taliqike formation, analyzed coal seams develop-ment and distribution under the sequence stratigraphic framework, summarized coal accumulation of Taliqike formation sequence stratigraphic model, and predicted the spatial and temporal distribution of coal resources. It was concluded that Taliqike formation could be divided into 2 sequences: SQ1 and SQ2; Seams mainly distribute in lake expanding system tract(EST)and highstand systems tracts (HST)of SQ1, SQ2; continuous coal developes both in EST and HST of SQ1 and SQ2, while coal in EST is better quality than that in HST.