喜山

燕山&喜山构造阶段过渡期郯庐断裂由左旋至右旋的转换，则导致了研究区断裂发育由NW向至NE（NEE）向的转型。

In the interim of Yanshan-Himalayan stage , the transition from sinistral to dextrorotation of Tanlu fault zone resulted in the transition of faults from NW-trending to NE ( NEE ) - trending in Zhanhua Sag .

烃源岩有机质丰度高，有机质类型主要为ⅡⅢ型，生烃期集中在喜山运动中晚期（E3N1）。

These source rocks are characterized by high abundance of organic matter with mainly type ⅱ - ⅲ . The major oil and gas generation stage of the Jurassic source rocks is between the Middle-Late episodes of the Himalaya Movement ( E 3 & N 1 ) .

研究表明，无论是煤，还是泥岩，库车坳陷三叠-侏罗纪烃源岩生气时间发生得晚，主生气期出现在10Ma以来的喜山期晚期，生气高峰期出现在5Ma之后。

It demonstrated that Triassic-Jurassic source rocks ( e.g.coal and mudstone ) in Kuqa Depression generated gas relatively later , which mainly occurred at the late stage of Himalayan Period ( after 10 Ma ) and main gas peak was in the last 5 Ma .

喜山运动使断陷盆地继续发展。

The Hemalaya movement promoted the fault & subsided basin to develope Continuously .

喜山期，氧化矿石形成。

The Oxidized gold ore was formed in Himalayan .

尤其以安县运动和喜山期运动为主。

County sports and especially Himalayan movement based .

盆地经历印支运动、燕山运动、喜山运动的改造。

This basin was reformed in Yinzhi movement , Yanshan movement and Ximalaya movement .

喜山运动表现为具有相当规模的滑移构造。

Xishan movement shows considerably scale slipping tectonic .

喜山运动中晚期活动控制构造圈闭的形成和发展；

Middle and late Himalayan movements determined the formation and development of structural traps .

烃源岩为寒武系&下奥陶统，成藏关键时刻在喜山期；

The source rock is the Cambrian & Lower Ordovician shale and shaly carbonate .

喜山早期黑云母花岗斑岩、强硅化花岗斑岩是区内斑岩型铜、钼矿床的成矿母岩。

The metallogenic rock are biotite and intense-silicified granite-porphyry of the early stage of Xishan .

川西坳陷喜山期构造应力场数值模拟及裂缝预测

Numerical simulation of Himalayan epoch tectonic stress field in West Sichuan depression and its fracture prediction

喜山期断裂、裂缝对致密储层储集性的改善作用。

And ④ an improvement on tight reservoirs by the faults and fractures occurred during Himalayan Epoch .

第一亚旋回末期的造山运动称为喜山运动。

The first , covering the time from late Cretaceous toPaleogene , is called the Himalayan Movement .

据地质和同位素年龄资料，推断走滑剪切运动发生在喜山期。

The geological data and isotopic dating suggest that the strike slip event took place during Himalayan movement .

滇西北宁蒗地区喜山期斑岩带形成的构造机制

The structural mechanism about the formation of porphyry belt during Himalayan period in Ninglang Area of Northwest Yunnan Province

渤海湾盆地经历了中新生代燕山、喜山期的强烈构造运动，构造格局错综复杂，前人对其成因解释亦是众说纷纭。

Bohai Bay Basin has experienced strong Yanshan , Himalayan tectonic movement , resulting in the complex tectonic framework .

因此，临南地区在燕山期和喜山期形成的圈闭是有利的煤成气勘探目标区。

The traps formed in Xishan and Yanshan periods are the favorable exploration target of coal-bed methane in the future .

塔里木盆地西南缘的构造变形是新生代喜山运动的产物，按变形卷入的深度及构造样式可分为两带：南带为前陆叠瓦逆冲－褶皱变形带.基底发生变形；

Structural deformation in the southwestern margin of the Tarim basin resulted from the Himalayan orogeny movement during Cenozoic era .

潜山内部层状油藏，主要接受晚期进油，储集空间以喜山期形成的裂隙为主。

The inner-buried hill stratigraphic oil pool receives late oil with fissures formed during Himalayan stage as reservoir space chiefly .

燕山&喜山期大幅度的抬升剥蚀使气藏被破坏形成了麻江古油藏。山西兴县奥陶系碳酸盐岩岩溶储层特征

Reservoir bed are karsts carbonate rock of Ordovician Honghuayuan . CHARACTERISTICS OF ORDOVICIAN CARBONATE KARST RESERVOIR IN XINGXIAN , SHANXI

早期喜山运动形成了该区主要构造的雏形，该期形成的古圈闭与生烃史配置良好；

The Early Himalayan Movement caused formation of main structions which has good correlation with maturation history of source rock .

盆地经历海西、印支、燕山、喜山多期次构造运动，是一个以中新生代为主体的经历了复杂演化历史的叠合性盆地。

Sangtanghu basin is a superimpose basin which deposited terrestrial sediments of Mesozoic Cenozoic and has a complicated structural evolutionary history .

喜山运动以后油气聚集的规律，受三组走向相互平行的北倾逆断裂所控制。

Oil and gas accumulation after Ximalaya movement was controlled by3 sets of north tilted reversed fault system with parallel strikes .

结果表明，燕山早期焉耆盆地处于弱挤压状态，构造变形量相对较小，而主要的变形量集中于燕山晚期和喜山期，并且喜山期变形稍弱于燕山晚期。

The results show that Yanqi basin is in weakly compressive status in early Yanshanian with smaller amount of structural deformation .

在第三纪的喜山期岩浆活动较强烈，因此，坳陷内第三纪火成岩分布广泛。

The Tertiary igneous rocks broadly distribute in this depression , since of magmatic activity was very frequent during the Xishan Epoch .

第6期（喜山晚期），主要为地下热液和埋藏有机溶蚀型岩溶。

In the sixth stage ( late Himalayan ), the main karst growth patterns are underground hydrothermal and buried organic corrosion karst .

北衙碱性斑岩型金矿床为“三江”地区金沙江&哀牢山喜山期富碱斑岩带中的重要金多金属矿床。

Beiya alkali porphyry Gold deposit is an important Gold poly metal deposit of the Jinshajiang-ailaoshan alkali porphyry zone in Sanjiang area .

本区新生代以来喜山运动等作用强烈，使得流体动力的构成、分布与油气成藏规律复杂。

Cenozoic Himalayan movement in the action such as strong , make the fluid dynamic structure , distribution and hydrocarbon accumulation rule complicated .

因此可将晚白垩世视为喜山期构造&岩浆阶段的开始。

Therefore , it appears to be considered the Late Cretaceous as the beginning of the tectonic magma cycle of the Himalaya stage .