褶皱带

华北陆台北缘晚元古代褶皱带变形&变质作用的显微构造研究

Microstructural Research on Deformation & Metamorphism of Late Proterozoic Fold Belt , North Margin of North China Platform

南极洲主要可分为东南极地盾及西南极中新生代褶皱带两大构造单元。

Antarctica can be divided into 2 big structural units , ie East antarctica shield and West Antarctica Mesozoic Cenozoic fold belt .

地槽褶皱带钙碱性安山流纹质火山岩有关的AgSnCuPbZn（Au）成矿亚系列；

Ag-Sn-Cu-Pb-Zn - ( Au ) subseries related to calc - alkaline basaltic - rhyolitic volcanic rocks of geosyncline (ⅳ);

结果表明GPS站主要运动方向为北北西，基本上与天山褶皱带走向正交，形成对天山的正向挤压。

The result shows that the principal motion is in NNW and generally orthogonal with the Tianshan fold belt , forming the squeeze to the Tianshan Mts.

当松潘-甘孜褶皱带受到D1-D2期缩短时，相邻的四川盆地并没有发生变形。

While the Songpan-Ganzi Fold Belt was subjected to D_1-D_2 shortening , the adjacent Sichuan Basin remained undeformed .

大巴山是NWWSEE走向的中央造山带中惟一的向南凸出大型弧型褶皱带，与秦岭&大别造山带的构造特征明显不协调。

The Daba Mountain , a unique convex-southern bow-like folding belt in NWW-SEE striking Qinling Orogen , is obviously uncoordinated with the Qinling orogenic belt in tectonic characteristics .

晚石炭世末期三叠纪东澳大利亚的鲍恩冈尼达悉尼（BowenGunnedahSydney）盆地系是位于拉克伦（Lachlan）褶皱带和新英格兰（NewEngland）褶皱带之间的一个长条形的构造盆地。

The latest Carboniferous to Triassic Sydney-Gunnedah-Bowen Basin System in the eastern Australia is an elongate structural basin that locates between the Lachlan Caledonian Fold Belt in the west and the New England Fold Belt in the east .

南部褶皱带表现为在大规模滑脱构造上（至少100km的水平滑移）的陆内浅部地壳变形。

Whereas that of the latter is represented by intracontinental , shallow crustal deformation on the basis of a large-scale detachment structure ( with a horizontal slip of at least of 100km ) .

东南则以右江褶皱带内的南盘江为界。统计表明，地震活动与南北带的速度结构相关：从20km以上的速度图象发现，大地震大都发生在高速和低速间的过渡条带上。

The statistical data show that seismic activity is related to the velocity structure of North-South zone : almost all of the major earthquakes took place in the transition strips between high-and low - velocity zones in the crust above 20 km .

本区北部伊犁地块基底岩石的Nd同位素模式年龄约为1.9Ga，南部南天山褶皱带的约为2.2Ga。

Nd isotopic model ages of basement rocks suggested that the crustal age of Ili plate in the north ( 1.9Ga ) is younger than that of the South Tianshan ( STS ) fold belt in the south ( 2.2Ga ) .

塔里木盆地与相邻褶皱带的区域构造演化

The regional tectonic evolution of Tarim Basin and adjacent fold belts

各排褶皱带均发育有生长地层及生长不整合，生长地层的开始沉积指示了该排褶皱和相应生长不整合的开始形成。

In each of such zones there are growth strata and growth unconformities .

徐州地区冲断褶皱带研究

A preliminary study on the thrust and fold belt of the Xuzhou region

天山褶皱带花岗岩类岩石的成因类型及构造环境的初步探讨

Preliminary study on the GRANITE-GENESIS types and tectonic environments of Tianshan Folded Zone

辽吉朝褶皱带古元古宙岩浆核杂岩及其大地构造意义

Magmatic core complex in the Liaoning-Jilin-Korea Paleoproterozoic fold belt and its tectonic significance

论文提出两种天然气成藏模式：一是川中斜坡带天然气聚集成藏模式，一是川中东部褶皱带天然气运聚成藏模式。

There are two kinds of gas accumulation models in the Upper Triassic .

川东侏罗山式褶皱带形成时代：不整合面的证据

The Folding Time of the Eastern Sichuan Jura-type Fold Belt : Evidence from Unconformity

辽东古元古宙褶皱带变质角闪质岩石的流动与变形机制

Flow and Deformation Mechanisms of Hornblende Rocks from the Paleoproterozoic Fold Belt in Liaodong Peninsula

东秦岭褶皱带河南段发现超大型金红石矿床

Rutile Ore Deposit Found in the East Qingling Fold Belt in Henan Province , China

巴楚隆起和柯坪冲断褶皱带是塔里木盆地西北部的两个构造单元。

The Bachu and Kalpin structural belts were two tectonic units in the Tarim Basin .

金衢盆地发育于浙西钱塘台拗和浙东华夏褶皱带接洽部位，受北东向和东西向断裂联合制约。

Jin-Qu Basin is situated at the junction of west-Zhejiang Qiantang syncline and east-Zhejiang folded zone .

中国中西部前陆冲断褶皱带油气地质条件及勘探建议

Petroleum geologic conditions in foreland thrust fold belts in west central China and proposals for exploration

把制服弄得多没褶皱带扣擦得多有光泽这都不够

or pressing your uniform or polishing your belt buckle , it just wasn 't good enough

福建省长乐南澳断裂带、平潭东山褶皱带基本特征的研究

Study on the Basic Characteristics of the Changle-Nan'ao Faulted Belt and Pingtan-Dongshan Folded Belt in Fujian Province

年轻的褶皱带等活动地区内部的密度值横向变化大。

And massif but the density horizontal change big inside the movable region of young fold band .

鄂尔多斯西缘逆冲褶皱带构造特征及其南北差异的形成机制

Tectonic Characteristics of the Western Ordos Thrust Fold Belt and the Causes for Its North South Segmentation

南天山库车冲断褶皱带构造变形时间&以库车河地区为例

The Time of Deformation on the Kuqa Fold-and-Thrust Belt in the Southern Tianshan-Based on the Kuqa River Area

对中国大地构造特点的一些认识并着重讨论地槽褶皱带的多旋回发展问题

On some of the tectonic characteristics of China with special discussion on the polycyclic development of geosynclinal FOLDBELTS

发育于蒙古弧形褶皱带的中生代沉积盆地群可分为残余海盆地、前陆盆地、裂陷盆地三种类型。

The Mesozoic basins of Mongolia can be classified into residual sea basins , foreland basins and rift basins .

乌鲁木齐山前坳陷逆断裂-褶皱带及其形成机制

Reverse fault and fold zone in the Urumqi range front depression of the Northern Tianshan and its genetic mechanism