carboniferous

an important memoir on Carboniferous crustacea.

有关炭纪甲壳动物的重要专题学术论文。

the shales are overthrust by Carboniferous rocks.

页岩层被炭层逆掩。

The allochthon consists of the Presinian,Sinian and Cambrian system.The autochthon comprises the Devonian and Carboniferous system.

推覆构造的外来系统为震旦系、震旦系和寒武系，原地系统为泥盆系和炭系。

The zimenqiao Formation silicolites of Lower Carboniferous is the country rock of Changkeng Au-Ag deposit.

下炭统梓门桥组硅质岩是粤西长坑金银矿床的直接容矿岩。

The study of reef-buiding biont of the Late-Carboniferous in Southern Guizhou rely mainly on alga,such as phylloid-algal and siphonopore algal.

黔南晚炭世生物礁造礁生物研究主要以藻类为主，藻、管孔藻等。

The deformation belts are formed by Late Carboniferous rocks, mainly mylonitization volcanic rocks and volcanic clastic sedimentary rocks.

变形带由下炭统干墩组组成，为一套糜棱岩火山岩、火山碎屑沉积岩。

Volcanicity was violent during the Early Carboniferous in Santanghu region.The volcanic rocks consist of basalts,andesites and dacite liparite,with andesites playing the main part.

三塘湖地区早炭世火山活动强烈，发育以安山岩类为主的玄武岩、安山岩、英安流纹岩的岩组合。

Recently some Brachiopoda, coral, gastropoda, phytolite is identified by Nanjing Institute of Geology and Palaeontology China Academy of Sciences.The age belongs to Late Carboniferous epoch.

在该地层中发现了一些腕足类、珊瑚、腹足类、植物，经中国科学院南京地质古生物研究所鉴定，时代属晚炭世晚期。

The paleo -geotemperature that Carboniferous went through at geologic history could not be too high and commonly was under120℃.The highest geotemperature occurred at late Cretaceous when la...

结合盆地地质情况,炭系在地质历史上经历的古地温不会太高,一般没有超过120℃,所经历的最高地温时间是晚白垩世,大量有机质在这一时期进行生排烃,具有晚期成烃的特点。

The deformation belts are formed by Late Carboniferous rocks, mainly mylonitization volcanic rocks and volcanic clastic sedimentary rocks.

变形带由下炭统干墩组组成，为一套糜棱岩火山岩、火山碎屑沉积岩。

Recently some Brachiopoda, coral, gastropoda, phytolite is identified by Nanjing Institute of Geology and Palaeontology China Academy of Sciences.The age belongs to Late Carboniferous epoch.

在该地层中发现了一些腕足类、珊瑚、腹足类、植物，经中国科学院南京地质古生物研究所鉴定，时代属晚炭世晚期。