Systematic study of the Mesozoic source rocks in the Qiangtang Basin.
系统地整理、分析、研究了羌塘盆地中生界烃源岩的特征。
Suggests that the Xijir Ulan structure belt is splitting from Qiangtang massif.
说明西金乌兰构造混杂带是羌塘陆块上裂解形成的。
The Cenozoic internal deformation in Qiangtang and Lhasa terranes is not serious.
拉萨地体和羌塘地体新生代内部变形较小。
The human activities are the essential causes of land use change in Qiangtang River Basin.
人类参加的经济社会活动是流域内土地利用变化的根本原因。
The Cenozoic volcanic rocks in Huochetou mountain, North Qiangtang can be divided into two different series.
藏北羌塘火车头山新生代火山岩可区分为钙碱性及碱性两个不同的系列。
The salt-related tectonics in the Qiangtang basin mainly formed in late Jurassic and was further patterned during Cenozoic.
羌塘盆地盐相关构造形成于侏罗纪末并在新生代进一步定型。
From the view of sedimentary and geochemistry, the characteristics of hydrocarbon generation in the Qiangtang Basin have been analyzed.
本文从沉积、地球化学的角度分析了羌塘盆地的油气生成特征。
Tanggulashan area may provides both Qiangtang area and Changdu area with important reference material through researching its sedimentary environment.
研究这一地区三叠纪地层沉积环境，可为进一步研究对比羌塘盆地与昌都地区地层沉积环境提供重要资料。
Paleomagnetic results from the both sides of Honghe fault zone have shown that the Yangzi block has been united with the Qiangtang terrane since Cretaceous.
红河断裂带两侧古地磁结果表明，羌塘地体与扬子地台至少从早白垩世以来已连接为一个整体。
The Qiangtang Basin in the hinterland of the Qinghai-Xizang Plateau is interpreted as a reworked basin which has undergone multiple phases of tectonic reworking.
位于青藏高原腹地的羌塘盆地是经历了多期构造改造的改造型盆地。
Qiangtang Basin is the largest and most prospective sedimentary basin of exploring for oil and gas in China Tethys structural domain, being a low exploration degree.
其中，羌塘盆地是中国特提斯域最大和最具有含油气远景的沉积盆地，该盆地勘探程度较低。
The basin swarm of the West Tethys belt, which is the richest petroleum-bearing region in the world presently, has a similar tectonic setting to the Qiangtang basin.
与其具有相似构造背景的西亚特提斯带盆地群是目前世界上油气最富集的地区。
There are several structural layers in the Qiangtang basin owing to multi-stage tectonic movements, and these structural layers show different features of deformation.
羌塘盆地由于受多期构造活动的影响形成多个构造层，不同构造层的变形特征存在明显差异。
At last, according to the palaeogeography characteristic and sedimentary evolution model, the general sedimentary facies model of Jurassic in Qiangtang basin was founded.
根据羌塘盆地侏罗系古地理特征及沉积演化模式，建立了适合于本区的侏罗系综合沉积模式。
The deep magnetic field characteristics in Qiangtang basin and Cuoqin basin of Qinghai-Ti-bet plateau is presented and analyzed by means of viewpoint of buried aulacogen.
介绍了青藏高原羌塘盆地和措勤盆地的深部磁场特征，用隐伏裂陷槽的观点分析了这些特征。
It firstly proposed that the Chaidamu tiny plate was affected by the Tarim plate in Mesozoic Era, but it was mainly influenced by Qiangtang plate and the south plate in Cenozoic Era.
本文首次提出了柴达木微板块在中生代主要受塔里木板块的影响，而新生代主要受羌塘板块及其以南板块的影响。
According to the observed and measured data of fluid inclusions in the Qiangtang Basin in this paper, the main types and characteristics of fluid inclusions were studied comprehensively.
该文根据羌塘盆地流体包裹体观察测试资料，对流体包裹体的主要类型和特征进行了综合论述。
Characteristics of Diagenetic evolution of clastic reservoir in the upper and middle Jurassic in Qiangtang basin are studied using data from chemical examination and reservoir measurement.
运用分析化验、储层测试等多种资料，对羌塘盆地中上侏罗统碎屑岩储层的成岩演化特征进行了研究。
According to the sedimentological evidences the paper believes that Qiangtang basin was a continental marginal basin during middle Jurassic time and was at an extensional architectonic setting.
论文用沉积学证据论证了羌塘盆地中侏罗世时期的盆地性质为陆缘盆地，存在于伸展性的大地构造背景。
In the west and central profile, the structure of the south Qiangtang depression is similar to the deep structure of the west uplift, featuring a double-layer intracrustal low-resistivity zone.
西部隆起区结构独特，浅中部与深部结构有别，存在一南倾低阻异常带。
The discovery of Ordovician-Devonian biotas and strata provide new important evidence for the stratigraphic division and correlation and the study of the tectonic evolution of the Qiangtang area.
羌南地区奥陶纪—泥盆纪生物和地层的发现，为与邻区地层划分对比和探讨羌塘构造演化提供了重要依据。
The discovery of Ordovician-Devonian biotas and strata provide new important evidence for the stratigraphic division and correlation and the study of the tectonic evolution of the Qiangtang area.
羌南地区奥陶纪—泥盆纪生物和地层的发现，为与邻区地层划分对比和探讨羌塘构造演化提供了重要依据。
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