晚石炭世 meaning in Chinese
late carboniferous epoch
Examples
- Evolution of junggar late carboniferous - permian foreland basin
准噶尔晚石炭世一二叠纪前陆盆地的演化 - The increasing volcanism implies that the regional tectonism became progressively severe from the early stage to late stage of the late carboniferous
自晚石炭世早期到晚期，火山活动期逐渐增长，休眠期逐渐缩短，反映出盆地性质自稳定向活动的转化过程。 - Started from benxi stage of late carboniferous , deposits of epiric sea were developed in this area along with the spreading of west - east direction and gentle depression of the basement
从晚石炭世本溪期开始，由于东西向拉张，基底缓慢下沉，本区广泛发育陆表海沉积。 - From the late carboniferous to the end of permian , the spores of the shishuyuan trough were from the north china province , and the marine sediments were absent in the southern part of eqm
晚石炭世至二叠纪末，柿树园海槽的孢子见于华北生物省，东秦岭南部缺乏海相沉积。 - The lamellibranchiiiata fossils and coral fossils of upper carboniferous period had been discoveried in the detrital rock and carbonafite rock by the geologic survey of the area of yishenjilike mountain
摘要通过对伊什基里克山特克斯达坂一带地质调查，首次于该区发现了一套含晚石炭世双壳、珊瑚、腕足及植物化石的碎屑岩。