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Huang Caoming, Zhou Qifeng. A PRELIMINARY STUDY ON SEDIMENTARY ENVIRONMENTSAND LOW OF COAL CONCENTRATION OF CARBO-PERMIANCOAL-BEARING SEQUENCES IN REGION OF COUNTY HUO,HUOXI COAL BASIN,PROVINCE SHANXI[J]. Acta Sedimentologica Sinica, 1988, 6(4): 72-80.
Citation: Huang Caoming, Zhou Qifeng. A PRELIMINARY STUDY ON SEDIMENTARY ENVIRONMENTSAND LOW OF COAL CONCENTRATION OF CARBO-PERMIANCOAL-BEARING SEQUENCES IN REGION OF COUNTY HUO,HUOXI COAL BASIN,PROVINCE SHANXI[J]. Acta Sedimentologica Sinica, 1988, 6(4): 72-80.

A PRELIMINARY STUDY ON SEDIMENTARY ENVIRONMENTSAND LOW OF COAL CONCENTRATION OF CARBO-PERMIANCOAL-BEARING SEQUENCES IN REGION OF COUNTY HUO,HUOXI COAL BASIN,PROVINCE SHANXI

  • Received Date: 1986-07-01
  • Publish Date: 1988-12-10
  • Huoxi coal basin is one of the six large coal basins in Province Shanxi. The study on sedimentary environments was carried out by complex methods including 55 isopach maps of main coal seams and sand bodies, a lot of trace elements analysis, X-ray diffraction analysis and DTA of clay minerals, rock identification under microscope, etc. The composition of coal-bearing sequencse, rock structur e probability cumulative curves of sandstone grain-size, electric log, analysis data of trace elements and the shape of coal seams and sand bodies are illustrated in detail. On basis of all these environmental criteria the coal-bearing formation was devided into six cycles and each environment was analysed. The middle Carboniferous Benxi Group is mainly lagoon-tidal flat deposits. The Upper Carboniferous Taiyuan Group is mainly lower delta-plain deposits. The lower Permian Shanxi Group is mainly upper delta-plain deposits. The thickness and distribution of coal seams are appe-arently controled by depositional environments. In this area,besides the good coal forming condition in environments of transition zone, as revealed by J.C. Home et al (1978), good coal forming condition exist in the environments of upper delta-plain and lago-ontidal flat too. There are two kinds of space relationship between the thicker belts of coal seam and the underlying sand body. First kind is superimposed position. Second kind is staggered position. First kind includes two varieties. One is coal seam formed on basis of tidal beach-barrier, the other is coal seam formed in environments of distributary mouth bar and distributary channel on lower parts of lower deltaplain. Second kind is coal seam formed in environments of distributary channel in transition zone and upper deltaplain. The thicker belts of coal seam and underlying sand body are in staggered position. The space relation-ship of thicker belts of coal seam and underlying sand body not only can play positive rolefor coal searching and exploration, and slso can serve as a new useful criterion for environmental analysis.
  • [1] 1.皮尔森,1970,测井资料地质分析,石油工业部石油勘探开发科学研究院情报室译,石油工业出版社

    2.刘宝裙主编,1979,沉积岩石学,地质出版社

    3.赖内克、辛格,1973,陆源碎屑沉积环境,石油工业出版

    4.Blatt, H.,et al.,1980, Origin of sedimentary rocks,Sed. Ed. Prentice- Hall,P. 136-144

    5.Donaldson,A.C.,1974, The Geo1.Soc.of Amer. Inc.Spec.paper, 148, p,47一78

    6.Glaister, R.P.and Nelsrn, H.W.,1974, Bull.of Canad.petrol.Geo1.V.22,N.3, p.203-240

    7.Horne, J.C.et al.,1978, Bull.of AAPG.V.62, N.12, p.2377-2411

    8.Reading, H.G.,1978, Sedimentary environments and facies, Blackwall Scientificpublications

    9.Reineck, H.G.and Singly I.B.,1980, Depositional sedimentary Environments, Sed Ea.,Springer-Verlag

    10.Staub, J.R.and Cohen, A.D.,1979, J.Sediment.Petrol.,V.49, N.1, p.133-144

    11.Visher, G.S:,1969, J.Sediment.Petrol.,V.39, N.3, p.1074-1106.
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  • Received:  1986-07-01
  • Published:  1988-12-10

A PRELIMINARY STUDY ON SEDIMENTARY ENVIRONMENTSAND LOW OF COAL CONCENTRATION OF CARBO-PERMIANCOAL-BEARING SEQUENCES IN REGION OF COUNTY HUO,HUOXI COAL BASIN,PROVINCE SHANXI

Abstract: Huoxi coal basin is one of the six large coal basins in Province Shanxi. The study on sedimentary environments was carried out by complex methods including 55 isopach maps of main coal seams and sand bodies, a lot of trace elements analysis, X-ray diffraction analysis and DTA of clay minerals, rock identification under microscope, etc. The composition of coal-bearing sequencse, rock structur e probability cumulative curves of sandstone grain-size, electric log, analysis data of trace elements and the shape of coal seams and sand bodies are illustrated in detail. On basis of all these environmental criteria the coal-bearing formation was devided into six cycles and each environment was analysed. The middle Carboniferous Benxi Group is mainly lagoon-tidal flat deposits. The Upper Carboniferous Taiyuan Group is mainly lower delta-plain deposits. The lower Permian Shanxi Group is mainly upper delta-plain deposits. The thickness and distribution of coal seams are appe-arently controled by depositional environments. In this area,besides the good coal forming condition in environments of transition zone, as revealed by J.C. Home et al (1978), good coal forming condition exist in the environments of upper delta-plain and lago-ontidal flat too. There are two kinds of space relationship between the thicker belts of coal seam and the underlying sand body. First kind is superimposed position. Second kind is staggered position. First kind includes two varieties. One is coal seam formed on basis of tidal beach-barrier, the other is coal seam formed in environments of distributary mouth bar and distributary channel on lower parts of lower deltaplain. Second kind is coal seam formed in environments of distributary channel in transition zone and upper deltaplain. The thicker belts of coal seam and underlying sand body are in staggered position. The space relation-ship of thicker belts of coal seam and underlying sand body not only can play positive rolefor coal searching and exploration, and slso can serve as a new useful criterion for environmental analysis.

Huang Caoming, Zhou Qifeng. A PRELIMINARY STUDY ON SEDIMENTARY ENVIRONMENTSAND LOW OF COAL CONCENTRATION OF CARBO-PERMIANCOAL-BEARING SEQUENCES IN REGION OF COUNTY HUO,HUOXI COAL BASIN,PROVINCE SHANXI[J]. Acta Sedimentologica Sinica, 1988, 6(4): 72-80.
Citation: Huang Caoming, Zhou Qifeng. A PRELIMINARY STUDY ON SEDIMENTARY ENVIRONMENTSAND LOW OF COAL CONCENTRATION OF CARBO-PERMIANCOAL-BEARING SEQUENCES IN REGION OF COUNTY HUO,HUOXI COAL BASIN,PROVINCE SHANXI[J]. Acta Sedimentologica Sinica, 1988, 6(4): 72-80.
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