Orogen相关论文
The timing of continental collision between India and Asia has been controversial for a long time because of the difficu......
Based on 40Ar-39Ar results of hornblendes and biotites and fission track dating results of apatites separated from the s......
A tectonic facies investigation carried out in the West Kunlun, China allows us to have worked out a tectonic model of o......
Geological and geochemical character and genesis of the Jinlongshan-Qiuling gold deposits in Qinling
The Qinling Carlin-type gold deposit belt is the second largest Carlin-type gold ore concentrated area in the world and ......
Geochronological constraints on 140-85 Ma thermal doming extension in the Dabie orogen, central Chin
Regional architecture of geochronology and differential cooling pattern show that the Dabie orogen underwent a thermal d......
Qinling-Dabie orogen 是一条重要的构造的带那趋势东方西方并且把大陆人中国划分成北、南部的部分。由于它的强壮的变丑，复杂结构，......
Trace elements in volcanic rocks from Yangba Formation, Bikou Group, Qinling area, China——Implicatio
YANGBA Formation of Bikou Group is located in south Qinling, a famous orogenic belt separating Chinesecontinent into tw......
The geological and paleomagnetic investigations suggest that the blocks in South China, except for those rifted from lat......
K-Ar dating of late Mesozoic volcanism and geochemistry of volcanic gravels in the North Huaiyang Be
Two eruption episodes are identified through systematic field investigations and K-Ar dating of the late Mesozoic volcan......
Mineralogical feature and geological significance of muscovites from the Longyuanba Indosinian and Y
Emplacement P-T condition estimations using granites are important for understanding metamorphic and erosional processes......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
赛坝沟地区的金矿床主要受近平行展布的嘎顺-乌达热呼韧性剪切带控制，区内金的活化、迁移受控于与矿床所在韧性剪切带，金矿体主要赋......
龙门山造山带属青藏高原东缘的陆内造山带，是一个建立的地层复合体，地层记录具有复杂性、混杂性、不连续性，不完整性和分带性等特征；根......
黔东南地区昔称雪峰隆起，属扬子地台次级构造单元江南台隆的西段。自70年代引进关籍华人比较大地构造学家许靖华远程推覆构造理论后......
大别山造山带，是秦岭褶皱带南东的组成部分，它与龟（山）-梅（山）断裂带、北东向断裂共同控制着豫南岩浆岩的分布。燕山期的中酸性岩基是成......
环斑花岗岩是一种特殊结构的花岗岩类,并且多数产在元古宙克拉通中.笔者曾报道了在秦岭造山带中发育有印支期具有环斑结构的花岗质......
回顾了逆冲楔临界角模型的发展,总结了影响逆冲楔临界角变化的诸多因素.这些因素并不是彼此独立地影响逆冲楔的运动和变形,而往往......
