1.
LITHOFACIES AND BIOFACIES OF LATEST PERMIAN AND EARLIEST TRIASSIC AT THE BORDERING REGION OF JIANGSU, ZHEJIANG AND ANHUI PROVINCES
苏浙皖地区二叠纪末、三叠纪初的岩相和生物相
2.
The study of the ecosystems in the survival and recovery time in the Early Triassic following the end-Permian mass extinction becomes a hotspot.
二叠纪末大灭绝之后，三叠纪初残存期和复苏期生态系研究成为当今热点。
3.
Sediments associated with the Great Dying became our next focus.
与二叠纪末期大灭绝有关的沉积层，成为我们下一个研究目标。
4.
At the end of the Permian period 225m years ago, between 80 % and 96 % of all living marine species were extinguished.
2.25亿年前的二叠纪末期，当时80％到96％的海洋物种灭绝；
5.
Calcimicrobialites after End-Permian Mass Extinction in South China and Its Implication of Paleo-environment;
华南二叠纪末大绝灭后的钙质微生物岩及古环境研究
6.
Taxonomy and Evolution of Brachiopods from Deep-water Facies in the End Permian in South China
二叠纪末深水相腕足动物群分类学与更替规律研究
7.
The Classification and Evolvement of Siliceous Spicules and the Cause of the Extinction during the End-Permian
华南二叠纪末硅质海绵骨针分类、演化及灭绝原因
8.
OSTRACODS FROM THE UPPERMOST PERMIAN SILICEOUS AND MUDDY ROCKS OF GUIZHOU, GUANGXI AND ANHUI
黔桂皖二叠纪末期硅泥质岩相地层中的介形类(英文)
9.
Some have suggested that cosmic dust is a better indicator of an impact event than fullerenes are.
其他人则追问：为什麽二叠纪末期岩层中的变形石英与铱含量都很少？
10.
These end Permian fullerenes are also associated with shocked quartz, another direct indicator of impact.
与这些二叠纪末期富勒烯一齐发现的，还有变形石英，即另一个撞击的直接遗迹。
11.
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。
12.
The Closure Time of the Paleo-Asian Ocean and the Paleo-Tethys Ocean:Implication for the Tectonic Cause of the End-Permian Mass Extinction
古亚洲洋和古特提斯洋的闭合时代——论二叠纪末生物灭绝事件的构造起因
13.
Anthracolithic period
(即石炭二叠纪) 大石炭纪
14.
Research on Conodont Evolution Across the Permian/Triassic Boundary in South China;
华南二叠—三叠纪之交牙形石演化研究
15.
This formation is dominated by a set of sandstone-mudstone dark clastic rock series which belongs to marginal marine deposit at the end of the Gondwana Carboniferous-Permian glacier period.
该组主要为一套砂岩－泥岩的暗色碎屑岩系，属冈瓦纳石炭－二叠纪冰川末期的边缘海沉积。
16.
by the end of the twelfth century
到十二世纪末的时候
17.
PERMIAN AND TRIASSIC TURBIDITE AND ITS TECTONIC SIGNIFICANCE IN THE NORTHWESTERN ZHEJIANG
浙西北二叠、三叠纪浊积岩系及其大地构造意义
18.
The granitic rocks in Zhuluke area, Western Liaoning, emplaced during Late Hercynian-Indosinian cycle, with Rb-Sr isochronal dating age of 226.8～260 Ma.
朱碌科地区花岗质岩石侵位时间为二叠－三叠纪。