| 释义 |
Tan-Lu fault
基本例句
郯庐断裂
The Tan Lu Fault zone experienced intense thrusting since Neogene.郯庐断裂带于新近纪以来呈现强烈的逆冲活动,使得先存的伸展性断层产生了一系列逆冲反转构造。
Mesozoic volcanic activities of the Tan Lu fault zone mainly appeared in Early Cretaceous and resulted in a set of volcanic rocks characterized by shoshonite series.郯庐断裂带中生代火山活动主要发生在早白垩世,形成了一套以橄榄安粗岩系为主的火山岩。
The Tan Lu fault zone turned into a huge extensional structure during Late Cretaceous to Eogene, leading to a series of development of fault bounded basins.晚白垩世 早第三纪郯庐断裂带转变成巨型的伸展构造 ,普遍控制发育了断陷盆地。
Magnetotelluric depth sounding sections of Tan - Lu Fault Zone and its crustal structure in Shandong, Jiangsu and Anhui Provinces郯庐断裂带鲁苏皖段大地电磁测深剖面与地壳结构
AN EARLY CRETACEOUS PULL APART BASIN IN THE MIDDLE SECTION OF THE TAN LU郯庐断裂中段的早白垩世拉分盆地 |