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Well-developed Neocene strata in western Qaidam Basin were a response to uplift of Qinghai-Tibet Plateau and their environmental changes.

柴西地区发育良好的新生代地层是对青藏高原隆升和环境变化的共同响应。

By above research, the following results are obtained.(1)The extracting module of aero-radioactive thematic information is integrated with ENVI, the remote sensing image processing software;(2) Based on the IDL, the computer program modules extracting following uranium thematic information have been developed, including initial uranium contents, active uranium contents, uranium migration coefficient, uranium information strengthen, uranium D-value and variance Ratio etc, al. Some of kalium special information extracting modules are also developed;(3)Based on the IDL, the aero-radioactivity information multi-parameter focus analysis module is developed;(4) It is proposed that a lots of phenomenon of uranium immigrating exist in Keping-Kuche are in the Neocene period. Because of the uranium pre-enrichment, the areas with high uranium content were formed in Neozoic and Quaternary. The above migration uranium are also the abundant source for uranium ore-forming in favorable strata of Mesozoic and Cenozoic system;(5)There are obvious uranium immigrating and enrichment in Eastern Portion of Keping Block Uplift, Yinate-Laolongjiang, and Qidaoban-KuChe.

通过上述研究,取得了如下成果:(1)实现了航放专题信息提取模块与ENVI遥感图像处理软件的无缝集成;(2)基于IDL语言开发了初始铀含量、活性铀含量、铀迁移系数、铀信息增强、铀差值方差比等航放铀专题信息,钾专题信息提取处理程序;(3)基于IDL语言开发了航放信息多参数聚焦分析处理程序;(4)发现柯坪-库车地区在晚第三纪开始出现了大量的铀迁移富集现象,不仅使上第三系、第四系沉积时因铀的预富集而形成铀含量高场区,而且也为研究区中新生代有利目的层的铀成矿提供了铀源条件;(5)研究认为,研究区柯坪断隆东段,英阿特-老龙江,七道班-库车等三个区块存在明显的铀迁入富集。

During the Cenozoic, the evolution of the sag might be divided into three stages: during the Eocene, because of regional extension effect of the NW-SE-striking, it was a ramp depression controlled by the Cangdong fault; during the Oligocene, it might have subjected to the combined effects of the NW-SE-striking regional extension and the dextral slipping of the NNE-striking deep fracture zone; during the Neocene and the Quaternary, though the regional extension had mainly stopped, the dextral slipping continued. Inside the slip zone, the local, SN-striking extension related to the dextral slipping became more and more apparent.

新生代演化分为3个时期:NW-SE向区域伸展作用,凹陷是一个由沧东断层控制的断坡凹陷;渐新世,凹陷受NW-SE区域伸展和NNE向深断裂带右旋走滑的共同作用;晚第三纪到第四纪,区域伸展作用基本停止,走滑作用仍在继续,由走滑作用导致的SN向局部伸展作用显得更加突出。

Comparison of tectonic evolutions and petroleum geological conditions in Tazhong and Tabei palaeohigh s in Tarim Basin;2. The palaeohigh in Junggar basin underwent multistage evolution from Neopaleozoic to Cenozoic, and four basic types such as successional, discontinuous, tilted and thrust ones were developed.

准噶尔盆地古隆起经历了自晚古生代至新生代的多期次演化,发育了继承型、间断型、掀斜型和冲断带型等4种古隆起基本类型,通过构造沉积演化及油气成藏分析探讨了陆梁隆起、莫索湾凸起、车莫隆起的油气勘探领域和勘探方向。

The two aspects of studies have made preparation necessary for the further studies of the evolution of Cenozoic tectonic deformation controlled by netlike plastic-flow in central-eastern Asia.

以上两个方面的研究,为中东亚地区网状塑性流动控制下新生代构造活动演变过程的进一步研究做好了必要的准备。

Fan-delta reservoir is one of important reservoirs in Meso-Cenozoic nonmarine basins China. It is significant to establish the relevant sequence stratigraphy method for evaluating and predicting fan-delta reservoirs.

扇三角洲储层是我国中、新生代陆相盆地重要油气储集层系类型之一,建立相应的层序地层学研究方法对于评价和预测扇三角洲相储层具有重要意义。

Tangyuan depression was a typical nonmarine fault basin in Paleogene, which was controlled by the faults and developed a variety of fractures with four directions in NE, NEE, EW and NW.

汤原断陷是典型的受断裂控制的新生代陆相断陷盆地,盆地内断裂非常发育,主要为NE、NEE、EW和NW四个方向。

The Garzê-Litang fault belt has experienced a series of complex evolutionary processes since the Paleozoic and is a large-scale, structurally complex ophiolitic mélange belt that has been strongly reworked and dismembered by overthrusting and sinistral strike-slip shear during the Cenozoic Himalayan orogeny.

提要: 甘孜—理塘断裂带自古生代以来经历了一系列复杂的演化过程,为一规模宏大、结构复杂并受到新生代喜马拉雅期逆冲推覆和左行平移走滑剪切作用强烈改造肢解的蛇绿混杂岩带。

However,the tectonic movement of the Tian Shan orogenic belt is the most intense.

天山造山带为中、新生代构造运动最强烈的区域。

Nominally anhydrous minerals, clinopyroxene, orthopyroxene and olivine, in peridotite xenoliths hosted by Cenozoic basalts from Panshishan, Lianshan and Fangshan of the Subei basin, eastern China have been investigated by Micro-FTIR for their water contents.

对来自苏北盆地盘石山、练山和方山地区新生代玄武岩中的50个橄榄岩包体矿物进行了系统的微区傅立叶变换红外光谱分析。

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