Discussion on the "Sedimentary Environment-Type of Coal-forming-Characteristic of Coal Quality" Rough Genetic Model I. Environment and Coal Facies
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摘要:
本文通过典型含煤段沉积成因标志的分析认为，南华北太原组属于比较典型的障壁岛─潮坪─泻湖成煤模式；山西组（P11）则属于比较典型的三角洲成煤模式，而华南龙潭组（P2）基本上代表了泻湖沉积相当发育的障壁岛─潮坪─泻湖成煤模式。在此基础上，根据反映成煤环境的综合标志（还原性质）的系列指标划分出三种四类基本煤相，即Ⅰ1─强还原型腐泥煤／腐殖腐泥煤煤相、Ⅰ2─强还原型富类脂组或富高氢镜质组的腐殖煤／腐殖腐泥煤煤相、Ⅱ─较强还原型腐殖煤煤相和Ⅲ─较弱还原型腐殖煤煤相。
煤的还原性（类型）具有既能表征成煤环境又可反映煤质特征的双重功能。正是通过煤的还原类型（即煤型）才把环境与煤质有机地联系起来，从而建立了沉煤环境－成煤煤型－煤质特征的成因模型。Abstract:Analyses of the deposit-genetic mark in typical coal-bearing members have shown that Taiyuan Formation （C2） in the southern part of North China represents a complete tidal flat-depositional system, consisting of subtidal flat （subtidal zone）, strand flat （intertidal lone-well developed） and supratidal flat （supralittoral zone）,which belong to the typical coal-forming model of barrier-tidal flat-lagoon.Shanxi Formation （P11） represents a comparatively complete delta-depositional regine,consisting of prodelta. delta front and delta plain, which belongs to the typical coal-forming model of delta. While longtan Formation （P2） in the South of china mainly represents the coal-forming model of barrier-tidal flat-lagoon with well developed lagoon deposit. Through the researches above, three kinds （four categories） of coal factes are devided based upon reductibility, which is the integrated mark of charactering coal-forming environment （by a series of indexes）. These coal facies with their character revealed respectively are I1-Sapropelic coals or humic-sapropelic coals of strong type-reductibility,I2-Humic coals or humic-sapropelic coal in rich-liptinites/rich-perhydrous vitrinites of strong type-reductibility,Ⅱ-Humic coals of stronger type-reductibility and Ⅲ-Humic coals of weak type reductibility,A series of indexes above contain total sulfur,index of ash composition,total iron,Fe++,B/ Ga,Sr/Ba,F/Cl,Palaeosalinity,isotopes of carbon,isotopes of sulfur,Eh,pH,alkane chromatography （the ratio of Aliphatic hydrocarbon to Aromatic hdrocarbon,carbon number of main peak,C21-/C2+ 21 and Pr/Ph）,biomarker of alkane （Quantity of terrigenous higher plants/amount of organisms source,Quantity of lower plants source/amount of organisms source,hepanes/terrigenous terpenoids and steroids/hopanes ratio） and biomarker of Aromatic hydrocarbon （dibenzothiopene/tri-fluorene and benezonthracene/chrysene ratio）.
Authers suggest that coals of different type-reductibility be characterized respectively by constituent of plants sources,organic and inorganic mather as well as properties of chamistry-technology-generating hydro carbon.Reductibility of coal （i.e. type-coal） may be of both characterizing coal-forming environment and feature of Quality-coal.It is by reductibility that environment is connected with Quality-coal.Therefore,the genetic model of environment-type-coal-Quality-coal build-up.
Authors thinks of coal-facies as total generality of sedimentary environment in peat-forming bog and must implicate environment,type-coal and Quality-except coal rank.
Authors advocate that from the point of view in practice（prediting environment and estimating Quality coal）,coal facies are researched and therefor,the regine of "practice coal facieology" should be set up,whose aim is to push the advance of coal-geology,coal-petrology and serve energy sources industry.
The study in this regine of both theoretical and practical importance. -
[1] 赵师庆，1981 ，中国华北东部晚古生代煤层的煤质差别和显徽特征，中国矿业学院学报，2期，41一53页 。 [2] 赵师庆，1984,我国腐殖煤的还原性质及其与沉积环魔的关系，沉积学报，2卷2期，53一64页 。 [3] 赵师庆、王贬字、刘德汉、盛国英，1987 ，不同煤相中煤和镜质组特征的初步研究，中国科学院地球化学研究所有机地球化学开放实验室研究年报，北京:科学出版社，23-44页。 [4] 韩德卑、任德贻、郭敏泰,1983 ，浙江长广煤川树皮残植煤的成因及其沉积环境，沉积学报，1卷4期4一14页 。 [5] 陈佩元、李小彦、高文生，1987 ，太原西山石炭二叠纪煤层煤岩特征及其成因分析，煤炭科学技术，6期（增刊），1一14页 。 [6] 陈家怀、陈善发、赵时久，1987 ，煤层巾硫同位素组成及成因探讨，煤田地质与勘探，5期，8一14页 。 [7] 李任伟、林大兴，1990，四川南桐地区二叠系龙潭煤层生物标记物及其地质意义，地质科学，2期113一126页 。 -
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