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塔里木盆地

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The multiple superpositional evolution of the Tarim basin is controlled by the wave prcesses of earth's crust, and the main cycles of these processes are 740~760Ma, 200~230Ma, 100~110Ma, 60~70Ma and 30Ma.

塔里木盆地的多期叠合发展受地壳波状运动的控制,控制塔里木盆地的主要周期有740~760Ma、200~230Ma、100~110Ma、60~70Ma、30Ma。

Based on the criterion of reliability of paleomagnetic data, we report the paleomagnetic data of Tarim, which was our achievement in past 10 years. Combined with the paleomagnetic results of other researchers, an integrated paleomagnetic data of Tarim, since Phanerozoic, is published here.

本文依据古地磁数据可靠性判别国际公认的一些基本原则,积集作者近年来在对塔里木盆地研究中获得的古地磁新成果,并结合其他学者发表的古地磁数据,编制了塔里木盆地显生宙以来的古地磁综合数据表。

There are abundant hydrocarbon resources in Silurian reservoirs in Tarim basin, and the stratum of the Silurian is the key exploration stratum in Tarim basin.

塔里木盆地志留系具有巨大的油气勘探潜力,是塔里木盆地当前重点勘探的目的层。

There are two branches stretched into China from Tethys during Cenomanian–Turonian in the Cretaceous, including the south branch, where occurred OAE2 in the Tibetan region, and north branch, where existed OAE2 in the southwestern of Tarim Basin too, thus it provided another evidence for OAE2's globality.

白垩纪Cenomanian-Turonian时期古特提斯海伸向我国的南北两个分支,其南支在西藏地区存在OAE2大洋缺氧事件,而北支在塔里木盆地西部也存在OAE2事件,这对丰富我国白垩纪事件研究、进行全球白垩纪OAE2大洋缺氧事件对比及其成因机制的探讨、查清塔里木盆地白垩纪古环境和烃源岩大规模形成的古气候控制因素以及白垩纪海相生物群演化、更替及其与重大地质事件的联系等具重要意义。

Directed under plate tectonics theories, author applied the relationship between orogenyy belt and basin, analyzation of proto-type basin restoration of Paleo-structures etc to systematically draw the Paleo-structural maps and Paleo-sedimental photographical maps on Z, O, S, D, C, P, T, J, K, E, N〓j, N1〓k, N〓k etc in Tarim basin.

以板块构造理论为指导,运用造山带与盆地、原型盆地分析、古构造分析等分析方法,系统编制了Z、O、S、D、C、P、T、J、K、E、N〓j、N〓K,N〓K等盆地及周缘古构造岩相图,全面系统地研究和恢复了塔里木大型叠合复合盆地构造演化历史,并将塔里木盆地构造演化史划分为7个构造演化阶段。

Summarizing the reservoiring courses of large and medium gas fields in China, they can be divided into 4 types...

目前中国天然气勘探的主要领域是:1中部、西部地区前陆盆地;2三大克拉通复合盆地(四川盆地、鄂尔多斯盆地、塔里木盆地);3近海的裂谷盆地和陆缘盆地

It is of great significance for the analysis of the petroleum accumulation and reallocation process in middle Tarim area as well as the whole craton area in Tarim Basin to correctly apprehend the petroleum accumulation conditions and model of Tazhong 4 Oilfield.

塔中地区是塔里木盆地重要的油气富集区,正确认识塔中4油田的油气成藏条件和成藏模式对于分析塔中地区乃至整个塔里木盆地台盆区的油气藏形成与改造均具有一定的意义。

It is of great significance for the analysis of the petroleum accumulation and reallocation process in middle Tarim area as well as the whole craton area in Tarim Basin to correctly apprehend the petroleum accumulation conditions and model of Tazhong 4 Oilfield.

塔中地区是塔里木盆地重要的油气富集区,正确认识塔中4油田的油气成藏条件和成藏模式对於分析塔中地区乃至整个塔里木盆地台盆区的油气藏形成与改造均具有一定的意义。

Whereas the seismic thermal lithosphere is about 150km thick, which means the Tarim lithosphere is not steady and became thinner. In this paper, writers analyzed the Tarim lithosphere thinning mechanism based on the tectonic thermal evolution quantitative method, and discussed three possibilities:the hotter India asthenosphere intruded under the Tarim lithosphere and made the Tarim lithosphere became unsteady;the bottom of Tarim lithosphere is heated by friction of the atheonosphere flow and washed off by the hot asthenosphere; the Xizang lithosphere delamination induced the convection, and the upflowing mentle heated the bottom of the Tarim lithosphere and make it enthinning.

本文利用构造热演化方法对塔里木岩石圈减薄的热演化过程进行了定量分析,探讨了塔里木盆地岩石圈减薄可能的三种机制:印度板块与欧亚板块碰撞后青藏高原岩石圈底部的软流圈较塔里木盆地岩石圈底部的软流圈的温度要高,青藏高原的软流圈地幔向塔里木盆地岩石圈底部侵入形成的热扰动使得塔里木盆地岩石圈底部的温度升高;塔里木岩石圈与其下流动的软流圈的摩擦剪切生热导致其岩石圈地幔底部温度升高,使得岩石圈底部发生热侵蚀,从而使得与软流圈接触的岩石圈地幔不断地加入到软流圈地幔;在塔里木盆地岩石圈的下部,青藏高原的岩石圈在该处发生了拆沉,从而诱发的软流圈地幔对流,上升的软流圈地幔流使得岩石圈地幔的温度升高而熔融,成为软流圈地幔。

This paper shows that crude oil in Tarim Basin possesses organic and inorganic binary genesis characteristics in accordance with the analysis of microelement and continental crust life matter.

本文通过对塔里木盆地石油中微量元素与陆壳生命物质的分析认为,塔里木盆地中的石油应具有有机和无机二元成因特征。

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