| 1. | 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 |
| 2. | 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。 |
| 3. | 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。 |
| 4. | 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。 |
| 5. | 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。 |
| 6. | The independent jiangda tectonic belt has appeared since late carboniferous , following the jinshajiang ocean crust of subducted beneath the changdu continental crust and the continental margin arc formed in east of changdu terrane
自晚石炭世金沙江洋洋壳开始向昌都陆壳地体边缘下俯冲，形成陆缘弧以来，独立的江达构造带就得以产生。 |
| 7. | The distributary channel microlithofacies evolution characteristics is studied with markov chain ' s analysis method , which lies in the shelf delta plain of dongzakou group of later carboniferous epoch in lixian county , gansu province
摘要采用马尔柯夫链分析方法研究了甘肃礼县地区晚石炭世东扎口组的陆架三角洲平原分支流河道微相演化特征。 |
| 8. | Dongtujinhe formation first been established in yining minor strata area , not only have an important value in stratigraphic correlation , but also proves that the yining basin similar as boluohuoluoshan blok in sedimentation and evolutionary process
东图津河组在特克斯盆地的首次确立，具有重要的地层对比意义，至少说明在晚石炭世伊犁盆地与博罗霍洛山地块具有相同的沉积作用及其构造演化特征。 |
| 9. | According to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field , including lithology , size distribution , sedimenta ry structure , geochemistry and paleontology etc . , the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt . it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal . the peat flat is the important paleoenviron ment for coal accumulation . the tidal channel destroys the coal bed . the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation
根据肥城煤田石炭系太原组的岩性、粒度分布、沉积构造、地球化学及古生物等沉积特征，将该区晚石炭世古地理划分为碳酸盐开阔台地和潮坪环境，认为太原组形成于潮汐作用为主的陆表海海岸，泥炭坪是成煤的重要古地理环境，潮渠对煤层有一定的破坏作用，地壳的脉动性振荡作用是控制沉积环境演化和聚煤作用的主要因素。 |
| 10. | Abstract : according to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field , including lithology , size distribution , sedimenta ry structure , geochemistry and paleontology etc . , the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt . it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal . the peat flat is the important paleoenviron ment for coal accumulation . the tidal channel destroys the coal bed . the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation
文摘:根据肥城煤田石炭系太原组的岩性、粒度分布、沉积构造、地球化学及古生物等沉积特征，将该区晚石炭世古地理划分为碳酸盐开阔台地和潮坪环境，认为太原组形成于潮汐作用为主的陆表海海岸，泥炭坪是成煤的重要古地理环境，潮渠对煤层有一定的破坏作用，地壳的脉动性振荡作用是控制沉积环境演化和聚煤作用的主要因素。 |
