首页|期刊导航|山东国土资源|内蒙古东胜煤田南部勘探区岩心地层划分及沉积环境

内蒙古东胜煤田南部勘探区岩心地层划分及沉积环境OA

Analysis on Stratigraphic Division and Sedimentary Environment of Cores in the Southern Exploration Areas of Dongsheng Coalfield in Inner Mongolia

中文摘要英文摘要

东胜煤田南部勘探区是揭示沉积环境与聚煤盆地形成演化的重要研究对象,对深化地质理论研究及指导煤炭资源勘探具有重要意义.本文根据研究区钻孔资料,采用岩性特征、标志层、层间距结合的方法,对延安组、直罗组、安定组、志丹群、第四系等各地层划分提出实际依据,对研究区含煤岩系特征及古地理环境和构造演化特征进行了探讨.研究结果表明:将沉积环境、古气候、盆地演化理论与实际工作中的岩心特征进行比对,从而采用综合方法进行地层划分,既有利于对各沉积环境和古气候影响下的岩心特征进行更加直观的认识和理解,又可以充分认识勘探区地层发育规律,进而取得准确的地质资料,为正确评估该区资源提供可靠的依据.东胜煤田经历了复杂的沉积过程,聚煤盆地多期的下降、抬升,形成了湖泊三角洲、河流等不同的沉积环境,控制了侏罗纪延安组煤层的形成.早侏罗世以来构造运动、沉积环境、盆地演化等因素控制了研究区地层、煤层发育.本研究成果为该区岩心地层划分及沉积环境对地层发育的影响提供了相关的理论支撑,为区域资源开发提供了一定的科学依据.

The southern exploration area of Dongsheng coalfield is an important research object for revealing the sedimentary environment and the formation and evolution of coal accumulating basins.It is of great significance for deepening geological theory research and guiding coal resource exploration.Based on drill-ing data in the research area,combining lithological characteristics,marker layers and interlayer spacing together,actual basis has been put forward for stratigraphic division of Yan'an formation,Zhiluo forma-tion,Anding formation,Zhidan group and Quaternary.Characteristics of coal bearing rock series,paleo-geographic environment and structural evolution have been studied.It is indicated that comparing the sedi-mentary environment,paleoclimate,basin evolution theory with the rock core characteristics in actual work,and using a comprehensive method for stratigraphic division,is not only beneficial for a more intui-tive understanding and comprehension of the rock core characteristics under the influence of various sedi-mentary environments and paleoclimates,but also for fully understanding the development laws of the strata in exploration areas.Thus,accurate geological data can be obtained.It will provide reliable basis for correctly evaluating the resources in the area.Dongsheng coalfield has undergone a complex sedimentary process.After multiple periods of decline and uplift in coal accumulating basin,different sedimentary envi-ronments,such as lakes,deltas and rivers have been formed,and controlled the formation of coal strata in Jurassic Yan'an formation.Since early Jurassic,tectonic movements,sedimentary environments and basin evolution have controlled the development of strata and coal strata in the study area.This research will provide theoretical support for the division of rock core strata and the influence of sedimentary environ-ment on strata development in the area,and a scientific basis for regional resource development.

宋文静;杨磊;陈晓波;房绍艳;杨建超;王永瑞;张燕妮

山东省煤田地质局第四勘探队,山东 潍坊 261206山东省煤田地质局第四勘探队,山东 潍坊 261206山东省煤田地质局第四勘探队,山东 潍坊 261206山东省煤田地质局第四勘探队,山东 潍坊 261206山东省煤田地质局第四勘探队,山东 潍坊 261206山东省煤田地质局第四勘探队,山东 潍坊 261206山东省煤田地质局第四勘探队,山东 潍坊 261206

天文与地球科学

岩心特征地层划分沉积环境东胜煤田内蒙古

Characteristics of coresstratigraphic divisionsedimentary environmentDongsheng coalfieldInner Mongolia

《山东国土资源》 2026 (3)

10-16,7

山东省煤田地质局科研专项,钻井液与小口径定向钻探的关系研究,项目编号:MTDZKY-2024-29

10.12128/j.issn.1672-6979.2026.03.002

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