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侵位于早—中石炭世。The emplacement age is the Early-Middle Carboniferous.
为主，确定其地质时代为早石炭世杜内期。The geological age is assumed to be Early Carboniferous Tournaisian.
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其时代为晚石炭世至早二叠世。The age of Kalagang formation of late Carboniferous was early Permian.
报道了甘肃北祁连走廊区早中石炭世的沉积特征。The flora which was found in Early Middle Carboniferous from North Qilian Z.
苏里格地区石炭-二叠系烃源岩广泛分布。The PermoCarboniferous source rocks are widely distributed in the Sulige region.
所发现的华北中、晚石炭世牙形石计有14属51种。There are in total 14 genera and 51 species of conodonts discovered in North China.
小兴安岭晚石炭世花岗岩具有明显的岩浆混合特征。Late Carboniferous granite in the Xiao Hinggan Mountains shows magma-mixing characteristics.
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山东淄博地区晚石炭世和早二叠世植物群由37属104种组成。Late Carboniferous and Early Permian flora is composed of 104 species in 37 genera in Zibo area.
其中海相地层中的主力烃源岩层为上震旦统和上古生界石炭―二叠系。The stratum of main source rock among the marine facies is the upper Sinian and the Paleozoic group.
断面上陡下缓，向下顺上石炭统太原组软弱层滑脱。The fault planes have a listric feature, slip-ped down along the soft layer of the Taiyuan Formation.
克孜尔塔格岩体侵入最新地层为下石炭统干墩岩组。The youngest strata intruded by the Kizil Tag intrusion are the Lower Carboniferous Gandun Formation.
上石炭统下部称泗峡口组，重新定义了泗峡口组的含义。The lower part of the Upper Carboniferous Series is called Sixiakou Formation whose definition differ.
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位于祁连山中段的肃南县法拉沟井田，含煤岩系为晚石炭世浅海型海陆交互相含煤建造。The coal-bearing rocks of the Falagou well field of Sunan County in the middle segment of the Qilianshan Mt.
河南省三门峡地区的铝土矿是赋存于中石炭统本溪组中的一水硬铝石型铝土矿。Bauxite of Sanmenxia area in Henan province is Al2O3·H2O and occurs in Benxi Formation of Middle Carboniferous.
济阳坳陷石炭二叠系烃源岩主要为煤和暗色泥岩。In the Jiyang depression, the main Carboniferous-Permian hydrocarbon source rocks are coals and dark mudstones.
新疆和田地区晚石炭一早二叠世沉积时期被面积广阔、水体较浅的陆表海所覆盖。The upper Carboniferous and lower Permian of Hetian in the south of Tarim Basin are deposited in the epeiric sea.
结合上述事实，通过沉积建造分析，该区在中石炭统曾存在沟弧盆体系。The analysis of sedimentary formation suggests the existence of groove-arc-basin system at the middle Carboniferous.
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早石炭世白山组火山岩是甘肃北山地区分布最为广泛的晚古生代火山岩。Volcanic rocks of early Carboniferous Baishan Formation were widely distributed in the Beishan area of Gansu Province.
矿田地层为泥盆系火山岩建造及下石炭统火山-沉积岩建造。The stratigraphy is shown as volcanic formations of Devonian and volcanic-sedimentary formations of Lower Carboniferous.
对采用微电解—白腐菌生物降解—石炭絮凝系统处理活性染料废水进行了研究。The treatment of dye wastewater by microelectrolysis white rot fungi degradation lime flocculation process has been studied.