构造的

High and extensive tectonic scarps play an important part in global morphotectonics, and are one of the basic tectonic landforms of the southern continental and subcontinental margins and transition zones between the continent and the ocean in the east of Asia.

高大并且广泛分布的构造悬崖是全球构造地貌的重要组成部分，是南方大陆和次大陆边缘的基本构造地形类型，同时也发育在亚洲东部的陆洋过渡区。

The Huade Group underwent at least two phases of deformation:the early phase of deformation gave rise to ENE-trending synclinorium and the late phase was marked by tectonic superimposition,forming NNW-trending folds. The main phase of deformation likely occurred in ~2.0 Ga B.P.The deformation of the Huade Group is related to a Paleoproterozoic orogenic event along the northern margin of the North China Craton, which has great significance for the study of accretion and breakup of the North China Craton.

化德群经历了两期构造变形，早期为北东东走向的复式向斜，晚期又遭受了构造叠加，形成了北北西向褶皱构造，其主期变形可能发生在2.0 Ga左右，它的褶皱造山是华北克拉通在古元古代向北增生的体现，这对研究华北克拉通的增生，裂解具有重要意义。

This thesis studies each structural layer's feature:(1) structural layer of basement:it is a Paleozoic folded basement,whose tectonic deformation and magma intrusion is fiercely,and it is affected by the early Hercynian tectonic movement and related to the underthrust and closure (C1) of Zhungaer ocean basin and the areal pressing of continents (C2-3);(2) structural layer of Permian:due to the regional extending and fault depression role in mid-Hercynian,it occurred to the combinations of structure and magma in Santanghu basin and it's periphery area,such as A-granite's stock,batholiths and diabase's dike.

二叠系构造层：受中海西区域性伸展断陷作用的影响，盆地及其周缘地区发育与伸展构造有关的构造-岩浆组合，如呈岩株、岩基状侵位的A型花岗岩以及呈岩墙状侵位的辉绿岩等。

The South China Sea is located at the junction of the Eurasian, the Pacific and the Indian-Australian plates, and it is one of the complex continental margins which are of active margin in early and passive margin in late. Five tectonic types of gas hydrate deposits including accretionary prism, fault-folded, dirpir, slide type and basin-edge slope are identified in the South China Sea.

南海位于欧亚板块、太平洋板块及印澳板块的交汇处，早期为活动陆缘，晚期演化为被动陆缘，其构造活动具有早期张裂、后期挤压的特点，这既不同于被动陆缘，也有别于活动陆缘，可视为&复合型&大陆边缘，兼具了&被动陆缘沉积速率高、活动陆缘构造活跃&的优点，从而形成了&增生楔型、断褶型、底辟型、滑塌型、盆缘斜坡型&等多种构造控制型水合物矿藏，是&复合型&大陆边缘水合物成藏地质模式的典型代表。

This ophiolitic tectonic melange is composed of some complex slabs from different tectonic settings and structural levels, which underwent different metamorphism with different PTt paths and reworking. The PTt path study in this paper reveals that Sanchazi metagabbro from Mian-Lue Suture zone of Qinling orogenic belt underwent two metamorphic and tectonic stages.

摘 要 勉略带是近年来秦岭造山带研究中揭示出来的代表晚古生代小洋盆的缝合带，组成复杂，它们经历了不同的变质、变形改造，构成了不同构造背景、不同构造层次、不同物质组成、具不同PTt轨迹的蛇绿构造混杂带。

This ophiolitic tectonic melange is composed of some complex slabs from different tectonic settings and structural levels, which underwent different metamorphism with different PTt paths and reworking. The PTt path study in this paper reveals that Sanchazi metagabbro from Mian-Lue Suture zone of Qinling orogenic belt underwent two metamorphic and tectonic stages.

勉略带是近年来秦岭造山带研究中揭示出来的代表晚古生代小洋盆的缝合带，组成复杂，它们经历了不同的变质、变形改造，构成了不同构造背景、不同构造层次、不同物质组成、具不同PTt轨迹的蛇绿构造混杂带。

In order to prvoide the new clue for the later tapping oil potential of maturing oilfiled, especially for the stratagem adjustment of high water-cut inefficient exploitation reservoir, and prolongate the realm and orientation of tapping oil potential, the waterflooding characteristics and the law of remaining oil distribution were studied.

结果表明，该块油层水淹程度仅80%左右，剩余油在平面上分布于区块的绝大部分区域，且与构造高低无明显关系，纵向上主要集中于层段的上部，尤其是位于该块西北区构造低部位的北断层区潜力单元，是与目前老油田潜力区主要局限于正向型微构造区所不同的新类型与新领域。

The major deposits in the Sanzhou ore field are related to Yanshanian or later tectonic activity,which is divisible into six sequences represented by:1the Upper Triassic-Lower Jurassic low-angle normal slip fault and associated structures near or immediately occurring on the unconformity between the Lower Carboniferous and the Upper Triassic;2the longitudinally bucking fold in Devonian-Carboniferous and Upper Triassic-Lower Jurassic strata;3the earlier phase thrusts toward northwest;4the transcurrent fault toward northeast;5the later phase thrusts toward northwest;and 6the extensional normal slip minor faults.

彭少梅 ，杨坤光，姚淑梅三洲矿田内主要矿床与燕山期或更晚的构造活动有关。燕山期构造活动可分为六个序列：1下石炭统与上三叠统不整合面附近和不整合面之上的上三叠统―下侏罗统中的低角度正滑断层及伴生构造，2泥盆系―石炭系及上三叠统―下侏罗统中的纵弯褶皱，3北西向逆冲断层，4北东向平移断层，5第二次北西向逆冲断层，6伸展性正滑小断层。

The fold cambers in plane which protrudes to the south. Regional tectonic pattern show bigger hiberarchy, which mainly is composed of roof -slippage-fault-fold. The tectonic pattern of shallow hiberarchy which includes middle-upper Triassic's fragmentary rock is fault-propagation and low-angle faults fracture, its roof rock is mainly pelyte. The tectonic pattern of midding-deep hiberarchy which includes upper Paleozoic's carbonatite is possibly thrust and broad-tempered fold.

研究区的构造样式表现出较大的层次性，总体为盖层滑脱式逆冲褶皱型，其中，以中、上三叠统碎屑岩为主的浅层次，其构造样式主要为紧密型断滑或断展褶皱低角度逆冲断裂，其滑脱面为三叠系下部泥质岩或粉砂质泥岩；以上古生界碳酸岩为主的中深层次，其构造样式推测以冲断和宽缓褶皱为主。

The verification and application of the formula show that the moderate tectonic intensity regions easily make for forming normal trap structures, the cap rock can be well preserved, and the transportation systems will be easily constructed.

构造强度中等地区由于易于形成一定规模的正向圈闭构造，封盖条件得以保证，同时有利于输导体系的建立，因此有利于油气藏的聚集和再富集；而构造强度过大和过小，则不利于油气的调整富集成藏。

Lugalbanda was a god and shepherd king of Uruk where he was worshipped for over a thousand years.

Lugalbanda 是神和被崇拜了一千年多 Uruk古埃及喜克索王朝国王。

I am coming just now,' and went on perfuming himself with Hunut, then he came and sat.

我来只是现在，'歼灭战perfuming自己与胡努特，那麼，他来到和SAT 。