| 1. | The mesozoic - cenozoic intracontinental strike - slip fault system and the associated hydrothermal uranium mineralization in the border area of eastern hunan and western jiangxi provinces
湘赣边区中新生代走滑断裂系统及对热液铀成矿作用的控制 |
| 2. | Tectonic - lithogenic - mineralogenetic epoch and its geologic history evolution indicate that intracontinental rifting stage ( t3 ~ e1 ) is the main metallogenic period of the jiangda tectonic belt
构造-成岩-成矿定年与地史演化研究表明，江达构造带主成矿期为陆内裂谷期。 |
| 3. | Himalayan orogen is by far the youngest and largest active continent - continent collision belt in the world and is the ideal place for studying the plate dynamics of intracontinental convergence and investigating the mechanism responsible for uplift of the plateau
喜马拉雅造山带是世界上目前仍在进行的、最年轻的、规模最大的陆-陆碰撞造山带，是研究陆内汇集过程板块动力学以及探讨高原隆升机制的理想场所。 |
| 4. | The collision between continental plates is a key to understanding the evolution of continental dynamics . perhaps the most spectacular large - scale result of plate tectonics is the broad complicated zone of intracontinental convergence between eurasia and peninsular india following their collision at about 45 ma
大陆内部的陆-陆碰撞过程是大陆动力学的核心问题，青藏高原被视为印度板块与欧亚板块于新生代碰撞的结果，是典型的陆-陆碰撞带。 |
| 5. | Four tectonic evolution phases have been made out in this area . they are original crust formed in the archean - early proterozoic era , continental crust shearing in the middle - new proterozoic era , plate tectonic developed in sinian - triassic period and intracontinental orogeny in the middle cenozoic period
将区内构造演化归纳为太古?早元古代原始地壳形成、中新元古代大陆地壳裂解、震旦?三叠纪板块构造体制、中新生代陆内造山等四个演化阶段。 |
| 6. | At last the rhythm of yanshanian volcanic rocks is classified into three series such as alkaline basalt , hkca , calc - alkaline shoshonite . 4 . based on the study of rock series , assemblage of igneous rock , characteristic of geochemistry , trace effect of isotope , the yanshanian volcanic rocks of yanshan - liaoning area are mainly calc - alkaline series , which should belong to the products of near continental margin of intracontinental tectonic setting
3 、在火山活动节律的划分、区域对比的基础上，研究了各级节律火山岩的岩石学、矿物学、地球化学和同位素地质学特征，将研究区燕山期火山岩划分为碱性玄武岩系列、高钾钙碱性系列和钾玄岩系列。 |
| 7. | Based on the analysis of the data on global metallogeny in the framework of geodynamics and study of the processes of continental evolution and metalloeny of of sanjiang , qinling and xingan - mongolia orogenic belts , we have reconsidered the geodynamic evlution and metallogeny during indosinian to early - yanshan movement in china , and established large - scale metallogenic model on intracontinental evolution we in orogenic belts . the main results are summarized as follow . ( 1 ) systematically gathering the data about large - scale and superlarge - scale deposits in the world and drawing up the map of global tectonics and metallogeny ; finding out the segmentation of circle - pacific ocean metallogenic belt and informing that the giant deposit clusters are the prominent feature of global metallogeny
本文在总结全球大规模成矿的地球动力学背景资料基础上，通过深入解剖和系统对比我国三江造山带南段、东秦岭造山带和兴蒙造山带中南部等典型造山带关键地区以陆内演化过程为核心的地球动力学演化历史及其成矿特征，重新认识了我国大陆印支?早燕山期的动力学演化过程及其成矿效应，建立了关于造山带陆内演化阶段主要过程中的大规模成矿模式。 |
| 8. | Yinggete - bagemaode metamorphic core complex belt with three - layer construction is put forward , which evolved from late jurassic to cretaceous . the extensional simple shear model of the chagan fault depression is established . the tectonic evolution and the dynamics character of chagan fault depression and its adjacent mesozoic - cenozoic basins are discussed : at the end of triassic continental orogeny increased crust thickness crust uplift and denudation were happened ; jurassic was a period of local partly extensional collapse of erogenic belt and cretaceous was a period of widely extensional collapse of postorogenic erogenic belt ; cenozoic was a period of the development of stable intracontinental depression with the character of long distant collision response and weaked compression flexure
讨论了查干凹陷及邻区中-新生代盆地构造演化及其地球动力学特征，三叠纪(印支期)为陆内造山作用与地壳增厚、隆升剥蚀阶段；侏罗纪(燕山早期)为造山后造山带的局部伸展垮塌阶段；白垩纪(燕山晚期)为造山期后大规模伸展垮塌作用与伸展盆地的发育阶段；新生代(喜山期)为远距离碰撞效应与弱挤压挠曲性质的稳定大陆内坳陷的发育阶段。 |
| 9. | A general survey of the formation , evolutionary histories of continental orogenic belts both in china and abroad reveals that orogenic belts have often undergone numerous and varied tectono - evolutionary stages , such as palaeocontinental break - up , ocean - land transition , continental matching - collision , intracontinental extension - basin - range coupling , and new tectonic uplift ( intracontinental orogeny ) , which are respectively accompanied by characteristic volcano - magmatisms
纵观我国以至全球的大陆造山带形成、演化历史，一个造山带往往经历了古大陆裂解、洋陆转换、陆块拼合碰撞、陆内伸展盆山耦合和新构造隆升（陆内造山）等众多不同的构造演化阶段，这些不同的构造演化阶段和不同的构造环境均有特定火山岩浆作用与之相伴。 |
| 10. | Scanning the formation - evolutionary histories of continental orogenic belts in both our country and whole workd , an orogenic belt has often undergone numerous and various tectono - evolutionary stages , such as palaeo - continental break - up , ocean - land transition , continental matching - collision , intracontinental extension - basin - range coupling , new tectonic uplift ( intracontinental orogeny ) , etc . , which are respectively companied with characteristic volcano - magmatism
纵观我国以至全球的大陆造山带形成-演化历史，一个造山带往往经历了古大陆裂解、洋陆转换、陆块拼合-碰撞、陆内伸展-盆山耦合和新构造隆升（陆内造山）等?多不同的构造演化阶段，这些不同的构造演化阶段和不同的构造环境均有特定火山岩浆作用与之相伴。 |
