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In the west and northwest heavy oil was reserved in the Hercynian , suffered from water washing and biodegradation while medium-light oil from Indo-Chinese episode and Yanshanian episode existed in the south and southeast of the oilfield.

塔河油田西部、西北部,保存了由海西晚期形成的遭受水洗氧化和生物降解的重质油;南部、东南部,主要保存的是印支—燕山期形成的轻—中质油。

Corbetts Tiger, or the Indo-Chinese Tiger, is found in Cambodia, China, Laos, Malaysia, Myanmar, Thailand and Vietnam.

科贝特斯虎(学名:Panthera tigris corbett)或印支虎,分布于柬埔寨,中国,老挝,马来西亚,缅甸,泰国和越南。

In the period of Mesozoic-Palaeozoic, Caledonian events and the evolution of Hercynian -early indo-Chinese cycle are experienced in two-phase marine passive continental margin and Craton basin in the lower and middle Yangtze Region, by which stable enormous thick Mesozoic-Palaeozoic deposites are induced, six sets of source rocks are produced, it has a strong capacity of hydrocarbon generation.

通过构造演化特征分析了海相烃源岩的发育,中、下扬子区中-古生代经历了加里东和海西-早印支旋回两个阶段的海相被动大陆边缘和克拉通盆地演化,形成了岩性稳定的巨厚中-古生界,发育了6套烃源岩,具有较强的生烃能力。

Meanwhile, the relict stratum of Jurassic in Shanxi and Henan Province can compare with the stratum in Ordos. So we can inferred from that the eastern boundary of the basin is on the east of Luliang Mountain. However, Taihang Mountain has already risen in Indo-Chinese epoch,so the farthest place of the east boundary can only be Taihang Mountain.

同时,山西和河南等地的侏罗系残留地层与鄂尔多斯可以进行对比,可以推断,盆地的东界在吕梁山以东,而太行山在印支期已经隆起,所以盆地的东界最远只能达太行山。

In Jurassic, the western, eastern and northern boundary of the basin had changed in varying degrees, except the south- Qinling orogenic belt rising in Indo-Chinese epoch, which is an always limited boundary. The western of the basin is limited by west-edge thrust nappe belt which formed in early and mid Jurassic.

侏罗纪时,除了盆地的南界为印支期隆起的秦岭造山带外——该造山带一直是一个限定性的边界,其他西部、东部和北部边界都有不同程度变化。

The limited hydrothermal karst and mixed zone beneath the anticline axis controls the porosity distribution of Ordovician System and it is anticipated that surroundings of the axis of fold formed by compressional reverse orverthrusting during Indo-Chinese epoch and the coordinated area of morphology of anticline in the screen of buried hill and that of top surface morphology is the best position for development of the reservoir.

局限的热液岩溶和裸露的背斜轴部之下的混合带对千米桥潜山奥陶系孔隙分布具有重要控制作用,预期在印支期挤压逆冲作用形成的背斜轴部,特别是潜山内幕背斜形态与潜山顶面形态相互协调的区域,应是储层发育最好的部位。

Then there was the victory of the Vietnamese red head, think of what Indo-Chinese Federation, had sent troops to fight in Cambodia, and China finally老大姐(then known as the Soviet Union more big brother, China老大姐) over a long face.

再就是越南人被胜利冲昏了头,想搞什么印支联邦,居然出兵去打柬埔寨,终于和中国老大姐(当时越人称苏联老大哥,中国老大姐)翻了脸。

Jurassic Tectonic Revolution in China and New Interpretation of the Yanshan Movement;2. The Indo-Chinese movement and Yanshan movement were two important tectonic movements in the Mesozoic era.

中生代印支运动和燕山运动是对济阳坳陷有重大改造的2次构造运动,印支期主要发育NW向逆推断层,燕山早期则为逆断层向正断层的过渡阶段,燕山中、晚期NW向断层发生构造反转,由逆断层转换为正断层。

Based on the analysis of tectonic deformation,extensional unconformity,sedimentary facies and paleogeographical rebuilding of southern Tibet,it is recognized that the extensional movement consists of active extension of Hercynian,Indo-Chinese and Early Yanshan epochs,and passive extension of the Himalayan epoch.

藏南特提斯域内伸展运动和伸展作用非常普遍,根据构造变形分析和伸展不整合、沉积岩相、古地理再造及岩相对比方法,对藏南海西期以来的伸展构造进行了较为系统的厘定,确定了海西期、印支期、早燕山期的主动伸展运动和晚燕山期和喜山期的被动伸展作用,并对这些运动特征进行了探讨。

East of the deposit is the famous Lincang-Menghai batholithic granite formed during Varisn to Indo-Chinese epoch which has a north-south direction of strike, west is Lancang grouup metamorphic rock.

矿体产在花岗岩与变质岩的构造破碎接触带中,成矿与花岗岩浆活动及大气降水所形成的流体作用有关。

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If you have any questions, you can contact me anytime.

如果有任何问题,你可以随时联系我。

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