扬子板块

大别一苏鲁造山带出露有世界上规模最大、保存最好的超高压变质地体，是三叠纪时扬子板块向北俯冲进入华北板块之下，而形成的大陆碰撞造山带。

The Dabie-Sulu orogenic belt , formed by the collision of the Yangtze craton and the North China craton in the late Triassic , has been know as the largest and best-preserved UHP terrane all over the world .

晚三叠世NW向逆推断层的发育为华北板块与扬子板块挤压拼接时产生的板内局部挤压调整效应；

The development of NW - trending reverse faults in Late Triassic was the local extrusion adjustment result of convergence of North China plate and Yangtze plate .

七·五计划期间，在扬子板块北缘地带所作地震测深（DSS）和大地电磁测深（MTS）成果揭示了该地带壳（慢）岩石圈结构，提供了分析古生代盆地形成演化的深部地质依据。

Deep seismic sounding and magnetotelluric sounding data revealed the crustal - mantle lithosphere structure on the northern margin of Yangtze plate and provided deep geological evidence for analysis of formation and evolution of the Palaeozoic basins .

扬子板块北部古被动大陆边缘的地球化学特征

Geochemical Characteristics of Ancient Passive Continental Margin of the Northern Yangtze Plate

扬子板块西北缘早志留世层序地层分析

Analysis of Early Silurian Sequence Stratigraphy at NW Margin of Yangtze Platform

柴达木-祁连-阿拉善为一楔状地块，来源于塔里木-扬子板块。

Qaidam-Qilian-Alxa as an integrated wedge-shaped block originated from the Tarim-Yangtze plate .

扬子板块板内构造形成机制浅析

Analysis on the Formed Mechanism of the Intraplate Tectonics in the Yangtze Plate

扬子板块俯冲的构造加积楔

Accretionary Wedge of the Subduction of the Yangtze Plate

华北板块和扬子板块碰撞时代的探讨

A discussion about the collision time between northern China plate and Yangzi plate

扬子板块东南大陆边缘晚前寒武纪热水沉积作用

The Late Precambrian Hot Water Sedimentation of the Southeast Yangtze Plate Continental Margin

加里东期扬子板块与华夏板块西南段分界线的岩相古地理制约

Lithofacies Paleogeographic Constraints of Southwestern Boundary between Yangtze and Cathaysian Plates in Caledonian

江南大地构造重新划分为三个I级构造单元：扬子板块、江南复合混杂岩带及华夏板块。

South China may be divided into three grade ⅰ tectonic units , i.

扬子板块的地壳演化与地层对比

Crust Evolution and Stratigraphic Correlation of Yangtze Plate

扬子板块石炭纪沉积层序及其全球性对比研究

Correlation of Carboniferous Depositional Sequences on the Yangtze Plate with Others on A Global Scale

鄂皖边界扬子板块前陆盆地的A型俯冲

A-Type Subduction of the Yangtze Plate Foreland Basin of in Anhui and Hubei Province Boundary

上扬子板块沉积改造金属矿床赋存深度问题的讨论

Discussions on the Problems of the Depth of Sedimentary Reformed Metal Deposits in Upper Yangtze Plat

三叠纪扬子板块的漂移导致下扬子区石膏、硬石膏矿床的形成

Formation of Gypsum and Anhydrite in Lower Yangtze Valley by the Drifting of Triassic Yangtze Plate

因此在约900-880Ma，在扬子板块东南缘的皖南地区出现过大规模的幔源岩浆活动。

900 to 880 Ma along the southeastern margin of the Yangtze plate in South Anhui .

成矿机制主要为扬子板块向北两次较大规模的俯冲所致。

Metallogenic mechanism mainly is that the Yangtze Plate happened to large scal underthrusts northwards at twice .

扬子板块东南大陆边缘上震旦统热水成因硅质岩的地球化学标志

Geochemical criteria of the Upper Sinian hydrothermal chert on the southeast continental margin of the Yangtze plate

川西元古代蛇绿岩与扬子板块西缘元古代造山带

Proterozoic Ophiolites in Western Sichuan and the Proterozoic orogenic belt on the west border of Yangtze paleo-plate

扬子板块东北缘首例独立铊矿床的初步研究

A preliminary study of an independent thallium deposit in Xiangquan on the northeast margin of the Yangtze block

扬子板块与华南板块对接带萍乡区段构造特征

Tectonic characteristics in the Pingxiang area in the junction belt between the Yangtze plate and South China plate

中国东部扬子板块同华北板块在中&晚三叠世拼接的沉积学证据

Sedimentologic Evidence on the Docking of Yangtse Plate and North China Plate in Middle-Late Triassic Period in East China

碧口地块位于秦岭大别、松潘甘孜造山带与扬子板块的交汇部位。

The Bikou terrane lies at the junction of Qinling orogenic belt , Songpan-Garze orogenic belt and Yangtze Plate .

扬子板块西缘北段新元古代花岗岩类的地球化学特征和成因

Geochemical Characteristics and Genesis of Some Neoproterozoic Granitoids in the Northern Part of the Western Margin of the Yangtze Block

研究区大地构造位置属扬子板块被动大陆东缘，松潘&甘孜造山带。

Tectonic position of the study area was located at the east margin of the passive continental of Yangzi Plate .

中元古代至早古生代塔里木板块与羌塘-扬子板块发生解体。

From the Middle Proterozoic to Early Paleozoic , the Tarim plate and the Qangtang-Yangtze plate were most probably disintegrated .

江南复合混杂岩带是扬子板块与华夏板块长期活动所致，构造极为复杂。

The tectonics of Jiangnan recombination melange belt is very complex resulted from long actuation of Yangtse plate and Cathaysian plate .

鄂皖边界大别南缘主俯冲边界断层的存在以及扬子板块前陆盆地盖层大型薄皮构造，揭示扬子板块向大别造山带之下的A型俯冲。

The main A-type subduction fault and large scale thin-skinned tectonics clearly reveal that the Yangtze Plate subsides towards Dabie orogenic belt .