• 基本释义

1.gas from coal measures
系地层气收藏指正
2.DEVELOPMENT AND TECTONIC SETTING OF THE ANYUAN COAL MEASURES IN CENTRAL JIANGXI
赣中安源系发育特征及构造条件分析收藏指正
3.Ccal-rich Belt and Synsedimentary Structure of Anyuan Coal Measures in Pingxiang Area
萍乡地区安源系富带与同沉积构造收藏指正
4.Probe into Depositional Characteristics and Environment of Late Triassic Anyuan Coal Measures,Jiangxi
江西晚三叠世安源系沉积特征及沉积环境探讨收藏指正
5.Study on the flora existing in the late Early permian coal measures in Fujian
福建早二叠世晚期含地层植物群的研究收藏指正
6.THE LATITUDE 38 N.TECTONIC BELT AND ITS CONTROLLING FUNCTION TO THE LATE PALAEOZOIC COAL MEASURES
38°构造带及其对晚古生代系的控制作用收藏指正
7.Since no fossils had ever been found in the coal measures in Renhe of Xiajiang county,Jiangxi Province,it was believed all along that it was part of the Upper Triassic Anyuan coal measures.
江西省峡江县仁和地区的系地层过去未获化石,长期以来,一直认为属上三叠统安源系。收藏指正
8.Study about Technique of Brightening of Flint Kaolin of Coal Measures in Carboniferous-Permian of Western Shandong
鲁西地区石炭二叠纪系硬质高岭土增白技术研究收藏指正
9.Analyses are made of the geological data available to indicate that in Anyuan Coal Measures development of synsedimentary structures governs the thickness, lithology and coal-bearing properies and the distribution of coal-rich belts, and also to show that these structures are responsible for the great differences in the coal measures of each mine in this area
本文着重通过对已有资料的分析说明,萍乡地区安源系同沉积构造发育,对安源系的厚度、岩相、含性及富带的分布起控制作用,同沉积构造还是使萍乡地区各矿区安源系彼此差异甚大的主要原因收藏指正
10.Discussion on thermal evolution and secondary hydrocarbon generation of organic matter from Upper Paleozoic coal measures in Huabei area
华北地区上古生代系有机质热演化与二次生烃探讨收藏指正
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