全部

1·Source beds are turbidite of middle Triassic series.

矿源层为中三叠统浊积岩。

2·The Lower and Middle Triassic rocks are uninterruptedly exposed in road cuts.

三叠系中下统沿着公路断面连续出露。

3·The Middle Triassic melange sedimentation is formed by the fault collapse in the platform.

中三叠世的沉积混杂作用形成于台内断裂塌陷；

4·Middle Triassic in Shaya Uplift and the adjacent area is one of important exploration targets.

塔北沙雅隆起及邻区的中三叠统可划分出披覆构造型勘探层。

5·It is suggested that Cerambycidae may originate at least before breakup of Pang-aea in Middle Triassic;

结果表明，天牛科的起源至少应追溯到三叠纪中期联合古陆分离之前；

6·In the region the Middle Triassic Anisic Stage stratigraphic development and facies variation are rather violent.

区内三迭系中统安尼·锡克阶地层发育，相变剧烈。

7·The comprehensive analysis indicated that Helanshan area was a part of Ordos Basin in the Early-Middle Triassic period.

综合分析结果表明，中生代早中期贺兰山地区是鄂尔多斯盆地的一部分。

8·There are complex and regular changes in depositional facies from the early to the middle Triassic strata in the Nanpanjiang Basin.

南盘江盆地的早—中三叠世地层中，沉积相形成复杂而有序的空间变化和时间变化。

9·It is regarded that Indosinian Movement took place from the later stage of Middle Triassic to the end of late Triassic about 180-220 Ma b.

认为印度运动发生在中三叠世晚期到晚三叠世末，距今180—220百万年，约经历了40百万年左右。

10·Like surrounding areas, the Jiangnan uplift belt in southern Anhui was situated on a passive continental margin during Sinian to Middle Triassic.

皖南地区的江南隆起带，在震旦纪—中三叠世与周边一样处于被动大陆边缘海相环境。