中三叠世

广西中三叠世沉积特征与微细粒金矿的探讨

On relation between the Middle Triassic sedimentary characteristics and the micrograined gold ore deposits in Guangxi

A型俯冲始自中三叠世末，延续到渐新世初，持续了约180Ma，主构造期为中三叠世末。

From the middle Triassic to the early Oligocene , the A-type subduction lasted about 180 ma and major tectonic stage is the middle Triassic . In the lower Yangtze region , there exist good oil generating , bearing and covering bed assemblages in the marine strata .

第一期变形（D1）发生在中三叠世，对应于造山带深俯冲的早阶段。

The first stage of deformation ( D1 ) corresponds to the early deep subduction stage of the orogenic belt in the Middle Triassic .

从而确定了本区中三叠世时的浊流主体流向为NW向，平均为300°。

Based on the above information , it is certified that the northwest averaging 300 ° is the main flow direction of the middle Triassic turbidite in the region .

2）新元古代－中三叠世，以现代板块构造体制为基本特征的板块构造演化（0.8～0.2Ga）；

Upper Proterozoic-Middle Triassic plate tectonic evolution featuring modern plate tectonic mechanism ( 0.8 ~ 0.2Ga );

贵州中三叠世拉丁晚期扬子台地边缘地表暴露带，经历的时间长，约1Ma（233～232Ma）；形成的厚度大（一般100～150m左右，最厚可达180m左右）。

The superficial exposure belt experienced a long evolutionary time ( about 1 Ma ), and formed a great thickness of sidiments ( usually between 100 ~ 150 m , with the largest thickness being some 180 m ) during Late Ladinian period of Middle Triassic .

其成因与深部地幔物质的不均一性及相关的运动状态有关，主要成生时限为早二叠世至早、中三叠世；

It resulted from the inhomogeneity and motion of upper mantle .

贵州兴义中三叠世Nothosaurus一新种

A new Nothosaur from Middle Triassic of guizhou , china

贵州福泉地区早、中三叠世沉积环境

Sedimentary Environments of Early and Middle Triassic of Fuquan Area , Guizhou

华北早中三叠世盆地恢复与古生界生烃

Reconstruction of Early-Middle Triassic basin in North China and hydrocarbon generation in Palaeozoic

下扬子盆地早、中三叠世古地理及其演化

The Early and Middle Triassic palaeogeography of lower Yangtze Basin and its evolution

扬子区晚二叠世&中三叠世海平面变化

Late Permian-Middle Triassic Sea Level Changes of Yangtze Platform

广西西部早、中三叠世牙形石序列

Early and Middle Triassic Conodonts Sequence in Western Guangxi

贵州贞丰发现中三叠世早期恐龙遗迹

The discovery of early Middle Triassic dinosaur trace fossils in zhenfeng , guizhou

南京地区中三叠世介形类化石及其意义

New recognition on Middle Triassic ostracods from the Nanjing area and their significance

贵州中三叠世岩隆沉积史及地球化学相

The development of the Middle Triassic buildup in Guizhou and its geochemical facies

广西早、中三叠世层序地层

Early and Middle Triassic sequence stratigraphy of Guangxi

桂西和黔南中三叠世珊瑚

Middle Triassic corals from W. Guangxi and s.guizhou

长江三峡东部地区中三叠世轮藻化石

Middle Triassic CHAROPHYTES in Eastern Yangtze Gorges Area

贵州中三叠世碎屑流

The Middle Triassic debris flows in Guizhou Province

黔西南地区早&中三叠世沉积岩相与LadinianCarnian期大海侵

Early-Middle Triassic sedimentary facies and ladinian-carnian transgression in southwestern Guizhou province , South China

湖北西部海相中三叠世介形类

Middle Triassic marine OSTRACODS FROM WESTERN HUBEI

湖南石门中三叠世巴东组轮藻化石

Middle Triassic CHAROPHYTES from shimen , Hunan

中三叠世的沉积混杂作用形成于台内断裂塌陷；

The Middle Triassic melange sedimentation is formed by the fault collapse in the platform .

四川早、中三叠世介形类

Early and Middle Triassic OSTRACODS FROM SICHUAN

大同三世和天演进化贵州中三叠世生物礁

Great Harmony , " Three Worlds " and Evolution THE MIDDLE TRIASSIC REEF IN GUIZHOU PROVINCE

中三叠世，伴随中特提斯洋开启，地壳拉张裂陷，兰坪&思茅中生代盆地开始形成。

The prototype basin was formed during the Middle Triassic accompanying the open of the Mid-Tethys Ocean .

贵州早、中三叠世台地&盆地相过渡区层序地层及沉积地球化学特征

Early Middle Triassic sequence stratigraphy and sedimentary geochemistry at the facies transition region in guizhou , China

造山类型的两次重大转换分别发生于早、中三叠世与晚白垩世。

The transfer of these orogenesis types occurred respectively in the early middle Triassic and late Cretaceous .

广西中三叠世沉积盆地是一个受晚古生代以来继承性断裂控制的断陷盆地。

The Middle Triassic sedimentary basin in Guangxi is a fault basin controlled by inherited rifts since Late Palaeozoic era .