准地台

贵州境内扬子准地台燕山期叠加褶皱特征

The Superimposed Fold Features of Yangtze Paraplatform of Yanshan Period in Guizhou

刘家坪杂岩体出露于扬子准地台西北边缘。

The Liujiaping complex occurs on the northwest margin of the Yangzi paraplatform .

扬子准地台区是本省地热异常的主要分布区。

Yangtze paraplatform is a major distribution region for geothermal anomaly .

关于扬子准地台西缘富锰矿的几个问题

Some Problems on High-grade Mn-Ores along the West Margin of the Yangtze Paraplatform

论扬子准地台西缘前震旦纪基底及其成矿作用

The Presinian basement on the western margin of the Yangtze paraplatform and its mineralization

对南黄海境内扬子准地台界限和演化的探讨

Discussion on the boundaries and tectonic evolution of the Yangtze paraplatform in the South Yellow Sea

扬子准地台西缘宝鼎断陷盆地层序格架下古地理演化与聚煤作用

Paleogeographical evolution and coal accumulation in a sequence stratigraphic framework in the Baoding fault basin of western Yangtze paraplatform

扬子准地台西南缘是我国重要的成矿区带。

The western rim of the Yangzi Paraplatform , is one of the most important metallogenic belts in the Southwest of China .

宁夏位于中朝准地台和昆仑秦岭地槽褶皱区两大地质构造单元的衔接部位。

Ningxia is situated on the border of two geological structure units which is Sino - Korean paraplatform and Qinling geosyncline folded belt .

（12±2）×10~6a的年龄值是攀西裂谷带内，甚至整个扬子准地台内最年轻的花岗岩年龄值。

12 ± 2 Ma is the youngest age for granitoids in the Panxi rift zone and even in the whole Yangtze Paraplatform .

本文对扬子准地台南缘一些地区和层段的含沥青砂岩的成岩作用进行了论述。

The diagenesis on the sandstones bitumen bearing in certain regions and sections of the southern margin , Yangtze Para-platform is discussed in this paper .

扬子准地台南缘下古生界生油岩无定型干酪根中有机质超微化石的发现及其石油地质意义

The discovery of organic Nanofossils in amorphous kerogen of Lower Paleozoic source rocks , southern margin of Yangtze para-platform , and its significance in petroleum geology

赣北地区属扬子准地台的一个组成部分，其地台盖层中的滑脱断裂与滑脱褶皱紧密伴生，共同构成滑脱构造。

Detachment fault were closely associated with detachment fold and they formed the detachment structure together in caprock of platform which is a part of Yangtz platform .

下扬子东南缘北段加里东期构造形迹新资料扬子准地台西北边缘地区地壳稳定性问题

New information of Caledonian tectonic features in the northern part of the southeastern margin of the Lower Yangtze valley Stability of the Northwest Edges of Yangtze Paraplatform

前新生代地层在海域以沉积岩为主，厚度大，时代全，主要为华北地台与下扬子准地台为背景的新生代沉积基础层。

About 50 % of exploration wells in Chinese offshore areas penetrated the Pre Cenozoic stratum which consists mainly of sedimentary rock with large thickness and different ages .

从地质与物探角度，论证川滇黔菱形地块可以构成扬子准地台西南缘一个Ⅱ级构造单元，范围较原“康滇地轴”稍有扩大。

According to the geological and geophysical characteristics , we prove that the Chuan-Dian-Qian rhombic massif is a ⅱ - order tectonic unit in the southwest margin of Yangzi paraplatform .

南黄海属于华北地台及扬子准地台的一部分，是一个由隆起、拗陷组成的中、新生代大型复式盆地。

The Southern Huanghai ( Yellow ) Sea is a part of the North China platform and Yangtze platform , and is a large Mesozoic and Cenozoic composite basin consisting of uplifts and depressions .

由软流层变化及断裂分布，认为扬子准地台和华南褶皱系两大构造单元的分界位于茶陵&永兴断裂附近。

According to the variation of the asthenosphere and the distribution of the fault system , it is suggested that the border between the Yangtze paraplatform and the Southern China fold system is near the Chaling-Yongxing fault zone .

江苏石油勘探局地质科学研究院，中国科学院南京地质古生物研究所.1988.江苏地区下扬子准地台震旦纪-三叠纪生物地层。南京：南京大学出版社。

Institute of geological sciences , Jiangsu Bureau of petroleum exploration and Nanjing Intitute of Geology and palaeonotology , Chinese Academy of sciences.1988.sinian-triassic biosratingraphy of the lower Yangtze paraplatform in the Jiangsu area . nanjing : nanjing University press .

宝鸡市大地构造位于中朝准地台与祁连褶皱系及秦岭褶皱系的交接部位，地质构造、地理环境复杂，属地质灾害多发、易发区，在未来地震作用下会诱发一系列的地质灾害。

Baoji situates at the junction of Sino-Korean paraplatform , Qilian fold system and the Qinling fold system . It has complex geological structure and geographical environment , which leads to an area with many and prone geological disasters , especially under the action of the next possible earthquake .

四川盆地位于扬子准地台西部，北邻秦岭褶皱带，西邻松潘甘孜褶皱带；它是上扬子准地台内通过北东向及北西向交叉的深断裂活动形成的菱形构造-沉积盆地。

Sichuan Basin is located in the western Yangtze Paraplatform , north of the Qinling fold belt , west of Songpan-Ganzi fold belt ; It is within the Upper Yangtze Paraplatform activity of deep faults which crossed by North East and North West formed the diamond-shaped formation of tectonic-sedimentary basin .

湖南省洞庭盆地位于扬子准地台江南隆起带的中段，前白垩纪是扬子准地台的组成部分，白垩纪第三纪成为断陷坳陷型内陆沉积盆地，古近系在全盆地分布广泛。

The Permian and the Paleogene sediments are major source rocks in the Dongting Basin which is located in the middle of the Yangzi Sub-plate in South Central China , prior to becoming an inland depression during the Cretaceous Paleogene .