1) Paleotethysides
古特提斯造山带
1.
The Indosinian foreland fold and thrust belt bordering Yunnan and Guangxi supported further evidence to the Paleotethysides.
滇桂交界处的印支期前陆褶皱冲断带为古特提斯造山带提供了进一步的证据。
2) Tethys tectonic zone
特提斯构造带
1.
In Mesozoic era, the formation and evolution of the Mesozoic Lanping Simao basin were controlled by the Tethys tectonic zone.
在中生代，该盆地的形成与演化受特提斯构造带的控制。
3) Atlas orogenic zone
阿特拉斯造山带
4) Palaeo-Tethys
古特提斯
1.
The study on the structure, volcanic sediment and magmatism shows that the east Kunlun Mountains belong to the Palaeo-Tethys active continental margin during the Hercynian-Indosinian period.
东昆仑地质构造特征、石炭—三叠系火山 -沉积建造及区域岩浆作用研究显示 ,海西 -印支期 ,该区属于古特提斯北侧活动陆缘的组成部分。
5) Paleotethys
古特提斯
1.
Four assemblages of radiolaria found in the formation data the sequence from late Late Permian to early Middle Triassic,which greatly changes the generally estimated progress schedule for the Paleotethys evolution.
地处古特提斯域的牡音河组是一套由放射虫硅质岩和凝灰岩组合而成、沉积速率极低的远洋沉积序列。
2.
SmNd isotopic constraints on the age of the BangxiChenxing ophiolite in Hainan Island: implications for the tectonic evolution of eastern PaleoTethys.;
本文将这些洋中脊型变质基性岩称之为“邦溪 -晨星蛇绿岩片”,它们与金沙江 -双沟 - Song Ma蛇绿岩在形成时代上基本一致 ,代表了东古特提斯洋的残片。
6) Paleo-Tethys
古特提斯
1.
The Wilson Cycle of the Jinshajiang Paleo-Tethys Ocean, in Western Yunnan and Western Sichuan Provinces;
滇川西部金沙江古特提斯洋的威尔逊旋回
2.
Triassic magmatism in the southern Lancangjiang zone,southwestern China and its constraints on the tectonic evolution of Paleo-Tethys
滇西古特提斯俯冲-碰撞过程的岩浆作用记录
3.
Paleomagnetic Constraints on the Closure Time of Paleo-Tethys:Implications for the Tectonic Setting of Formation of Triassic Songpan-Ganzi Flysch Complex
古特提斯洋的闭合时代的古地磁分析:松潘复理石杂岩形成的构造背景
补充资料：提婆菩萨造论
【提婆菩萨造论】
（书名）百字论一卷，百论二卷，外道小乘四字论一卷，外道小乘涅槃论一卷。
（书名）百字论一卷，百论二卷，外道小乘四字论一卷，外道小乘涅槃论一卷。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条