Metallogenesis of the Tibetan collisional orogen: A review and introduction to the special issue

Z Hou, NJ Cook - Ore Geology Reviews, 2009 - Elsevier
Mineral deposits associated with continental collision are abundant in many orogenic
systems. However, the metallogenesis of collisional orogens is often poorly understood, due …

Constraining the timing of the India-Asia continental collision by the sedimentary record

XM Hu, JG Wang, W An, E Garzanti, J Li - Science China Earth Sciences, 2017 - Springer
Placing precise constraints on the timing of the India-Asia continental collision is essential to
understand the successive geological and geomorphological evolution of the orogenic belt …

Triassic three-stage collision in the Paleo-Tethys: Constraints from magmatism in the Jiangda–Deqen–Weixi continental margin arc, SW China

B Wang, L Wang, J Chen, F Yin, D Wang, W Zhang… - Gondwana …, 2014 - Elsevier
Triassic volcanic rocks in the Jiangda–Deqen–Weixi continental margin arc (DWCA) in the
Sanjiang area of SW China formed as a result of the closure of the Paleo-Tethys and …

Granite, gabbro and mafic microgranular enclaves in the Gejiu area, Yunnan Province, China: a case of two-stage mixing of crust-and mantle-derived magmas

Y Cheng, C Spandler, J Mao, BG Rusk - Contributions to Mineralogy and …, 2012 - Springer
Geochronological, geochemical, whole-rock Sr–Nd, and zircon Hf isotopic analyses were
carried out on the Jiasha Gabbro, mafic microgranular enclaves (MME) and host Longchahe …

[HTML][HTML] 藏南扎西康大型铅锌银锑多金属矿床叠加改造成矿作用初探

梁维, 侯增谦, 杨竹森, 李振清, 黄克贤, 张松, 李为… - 岩石学报, 2013 - html.rhhz.net
扎西康铅锌银锑多金属矿具有多期多阶段的复杂成矿的特征. 结合对区域成矿带,
典型矿石结构构造, 闪锌矿Fe 含量变化, 金属成矿元素分带性以及流体演化特征的分析 …

鄂尔多斯地块南缘构造演化及其对盆地腹部的构造—沉积分异的效应

包洪平, 郭玮, 刘刚, 李磊, 武春英, 白海峰 - 地质科学, 2020 - dzkx.org
鄂尔多斯地块南缘处在盆地与秦岭造山带之间这一盆—山结合的过渡部位,
由于构造位置的特殊性, 自古生代以来其构造及沉积面貌与盆地腹部地区存在较大差异 …

[HTML][HTML] 滇西来利山花岗岩年代学, 地球化学特征及其壳源部分熔融成因

孙转荣, 董国臣, 赵作新, 王伟清, 刘圣强 - 中国地质, 2017 - cgsjournals.com
与锡矿有关的花岗岩成因一直是地学界关注的焦点. 来利山花岗岩位于云南省腾冲—
梁河地区(花岗岩带上), 构造上属于腾梁花岗岩带. 该花岗岩带总体呈北北东向带状展布 …

[引用][C] 青藏高原碰撞造山带: I. 主碰撞造山成矿作用

侯增谦, 杨竹森, 徐文艺, 莫宣学, 丁林, 高永丰… - 矿床地质, 2006

[引用][C] 印度大陆与亚洲大陆早期碰撞过程与动力学模型——来自西藏冈底斯新生代火成岩证据

侯增谦, 莫宣学, 高永丰, 杨志明, 董国臣, 丁林 - 地质学报, 2006

[引用][C] 初论碰撞造山环境斑岩铜矿成矿模型

杨志明, 侯增谦 - 矿床地质, 2009