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淮南煤田二叠系三、四含煤段古水系特征 被引量:3

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China
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摘要 本文通过对淮南煤田二叠系三、四含煤段5千余个钻孔资料的系统分析和煤矿开拓巷道中古流向的实际测量,获得大量有关古水系的第一性资料。研究认为可与现代珠江三角洲上的水系进行类比、进而推断三、四含煤段沉积时的环境为一种由多条陆源河流共同作用形成的复合型三角洲。 The Huainan Coalfield, covering an area of more than 8000 km2. is concealed by the Quaternary system, and the main coal-bearing strata are Permian Members C-D. By the investigation of more than 5000 bores and surveying of undergroud tunnels of the coal mines in the research district, many characteristics of the paleodrainage have been acquired as follows: 1. By undergroud surveying of the main channel sandstones of the members C-D, it is shown that during their deposition the paleocurrent direction is southward. Z.The paleodrainage of the Permian members C-D have two forms, the branched channel system (in member C) and the anastomosing channel system (in member D). The channels composed the drainages are very stable and fail to lateral migration. 3. The results of grainsize analysis and the C-M pattern of the same genetic increment demonstrates that the paleostream flown from north to south, and the south side is more near to the sea. 4. The characteristics of sedimentology and sedimentary geochemistry indicate that the fine sediments of member C which deposited in the branched channel system contain much more of the tidal sediments, burrows, and Lingula sp. etc. The content of the trace element B. B/ Ga and Ca/ (Fe+Ca) are higher than that of member D. To sum up the characteristics discussed above and analyze by means of Walther's Law of correlation of facies. and compare with the drainage on the modern Pearl River, the authers propose that the paleodrainage of the members C-D is more similar to that on the modern Pearl River Delta, that is to say, it can be divided into two parts, the anastomosing fluvial system near the continent and the branched fluvial system close to the sea. It is recognized that the paleodrainage discussed in this paper is different from that on the Mississippi River Delta and / or on the Yangtze River Delta, that could he account for which discussed in this paper is a complex delta formed together by several continental streams, the low-medium t rupge and the Coriolis force exist in the historv of the Earth.
出处 《沉积学报》 CAS CSCD 北大核心 1991年第3期1-10,共10页 Acta Sedimentologica Sinica
基金 国家青年科学基金
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二级参考文献2

  • 1蓝昌益,煤炭学报,1988年,1期,11页
  • 2黄镇国,珠江三角洲形成发育演变,1982年

共引文献10

同被引文献22

  • 1郭彦省,孟召平,杨瑞昭,张丽红,刘亚川,孙学渊,赵国平.地震属性及其在煤层厚度预测中的应用[J].中国矿业大学学报,2004,33(5):557-562. 被引量:32
  • 2蓝昌益,杨本才,彭苏萍,等.淮南煤田二叠系主要煤层的成煤环境[J].煤炭学报,1986,(1).
  • 3李金平,陈向阳,乔立湖.小区域地壳变形监测与分析研究[J].测绘工程,2007,16(4):41-44. 被引量:1
  • 4张鹏飞,中国沉积学,1993年
  • 5龙云作,海洋地质与第四纪地质,1989年,5卷,4期,49页
  • 6蓝昌益,煤炭学报,1988年,1期,11页
  • 7蓝昌益,1986年
  • 8彭苏萍,1986年
  • 9黄镇国,珠江三角洲形成发育演变,1982年
  • 10黄振国,热带地理,1981年,2期,50页

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