There are complex and regular changes in depositional facies from the early to the middle Triassic strata in the Nanpanjiang Basin.
南盘江盆地的早—中三叠世地层中，沉积相形成复杂而有序的空间变化和时间变化。
Source beds are turbidite of middle Triassic series.
矿源层为中三叠统浊积岩。
Nanpan River Basin experienced extension, fault depression in middle-late period of Early Triassic and compression fault rising after Ladinian of Middle Triassic.
南盘江盆地三叠纪，经历了早三叠世中、晚期的拉张、断陷和中三叠世拉丁期之后的挤压断隆。
On the southwestern margin of the basin there occur middle Yanshanian Late Triassic and Early Cretaceous coarse clastic molasse-like deposits and angular unconformity.
在盆地西南缘发育燕山中期的晚侏罗世和早白垩世的粗碎屑类磨拉石建造及其地层间的角度不整合。
Middle Triassic in Shaya Uplift and the adjacent area is one of important exploration targets.
塔北沙雅隆起及邻区的中三叠统可划分出披覆构造型勘探层。
The comprehensive analysis indicated that Helanshan area was a part of Ordos Basin in the Early-Middle Triassic period.
综合分析结果表明，中生代早中期贺兰山地区是鄂尔多斯盆地的一部分。
According to geological age, it may be divided into Upper Triassic coal-bearing formation and Lower-Middle Jurassic clastic rock formation.
根据它的地质时代，划分为上三叠统含煤建造和中下侏罗统碎屑岩建造。
Like surrounding areas, the Jiangnan uplift belt in southern Anhui was situated on a passive continental margin during Sinian to Middle Triassic.
皖南地区的江南隆起带，在震旦纪—中三叠世与周边一样处于被动大陆边缘海相环境。
The forming age of maximum sinistral strike-slip occurred in Middle-Late Triassic.
最大左行走滑活动时期当在中晚三叠世。
The Jialingjiang Formation distributed in northwestern Jiangxi has long been assigned to the Middle Triassic though no adequate fossil data have been obtained.
分布于赣西北地区的三叠系嘉陵江组，以往虽未获充分的化石资料，但长期以来把它划归中三叠统。
The north-south structure in upper triassic epoch and, 4) The whole tilting structure after middle jurassic epoch.
晚三迭世的近南北向构造和4）中侏罗世以来的整体掀斜构造。
The Lower Triassic carbonate bank section of Songshan, Wuxi is particular and typical in the Middle and Lower Yangtze Region.
无锡嵩山下三叠统碳酸盐浅滩相剖面在中下扬子区具有特殊性和代表性。
The diffraction hilly structures widely develop on the top of Middle Triassic and Lower Triassic in the seismic horizontal stacking time sections in the central part of Sichuan Basin.
在四川盆地中部的地震水平叠加时间剖面上，中三叠统及下三叠统顶部广泛发育绕射丘状结构。
The Middle Triassic melange sedimentation is formed by the fault collapse in the platform.
中三叠世的沉积混杂作用形成于台内断裂塌陷；
The accumulation mechanism of natural gas is still an unsolved problem in the Lower Triassic Jialingjiang Formation of Moxi-Longnüsi area in the middle of Sichuan Basin.
川中地区磨溪—龙女寺构造带下三叠统嘉陵江组天然气的成藏机理一直是一个悬而未解的问题。
Relating with the sedimentary environments, uranium mineralization is primarily occurred in the lower-middle Triassic and the base of Longtan Formation.
铀矿化主要赋存于下—中三叠系及龙潭组底部，和沉积环境有一定关系。
The gas generation center of the Middle-Upper Triassic gas kitchen lies in the Kelasu structural zone, gas generation intensity decreased far from the center.
中上三叠统气源灶以克拉苏构造带为生气中心，向四周生气强度逐渐变小；
The area of western Sichuan was situated in the southwestern part of an evaporative sea basin (Weixi area) during Leikoupo age in middle Triassic.
川西地区中三叠世雷口坡期位于威西蒸发海盆的西南部。
The Early - Middle Triassic short - term changes of Yangtze are briefly concordant with those of Haq's world curve, whereas its long-term changes are discordant.
扬子区早—中三叠世短期变化曲线与世界曲线一致，而长期曲线则不相符。
The Lower and Middle Triassic rocks are uninterruptedly exposed in road cuts.
三叠系中下统沿着公路断面连续出露。
During Middle Triassic, the Gejiu area was in a special sedimental environment, i. e. in a restricted marginal sea basin within the continental rift system.
中三叠世，个旧矿区处于特殊的沉积环境—陆裂谷系中的局限边缘海盆。
These evidences prove that the Early and Middle Triassic paralic and lacustrine features had already been inactive in the Middle and Late Triassic Ordos basin.
表明中晚三叠世鄂尔多斯盆地已经结束早中三叠世近海湖泊的性质。
During Late Triassic to Early Jurassic, Marine sediments formed (sallow_bay facies or alternating continent_marine facies), and only continental facies deposited during Middle Jurassic to Cretaceous.
上三叠统—下侏罗统有海相地层(浅海海湾相或海陆交互相碎屑岩)分布，而中、上侏罗统及白垩系为陆相地层。
The intrusive rocks from middle-late proterozoic to late triassic in middle-south Jiangxi province can be divided into two tectonic-magma areas of Wuyishan and south-west Jiangxi.
依据不同构造岩浆区单元，江西中南部中新元古代-晚三叠世的侵入岩可划分为武夷山构造岩浆区、赣西南构造岩浆区。
Analysis of the fossil associations of dasycladalean algae in the Middle and Upper Triassic of Croatia is given with the emphasis on the stratigraphical ranges of particular species and associations.
对克罗地亚中三叠统和上三叠统的粗枝藻属化石组合的分析，侧重于特定的种和相关化石的地层分布方面。
The solution void of analcites developed in the middle and lower sections of Karamay Formation and Baikouquan Formation in the Triassic.
由北向南方沸石溶蚀形成的孔隙呈现出发育带—较发育带—不发育带的趋势。
The sedimentary-subsidence center is located in Linqing-Dongpu-Taikang and Huainan-Huaibei areas, where the Middle-Lower Triassic is as thick as 2000~2600m.
中下三叠统沉积沉降中心位于临清-东濮-太康和两淮地区，沉积中心的中下三叠统厚度达2000～2600 m。
In the region the Middle Triassic Anisic Stage stratigraphic development and facies variation are rather violent.
区内三迭系中统安尼·锡克阶地层发育，相变剧烈。
The intrusive rocks from middle-late proterozoic to late triassic in middle-south Jiangxi privince can be divided into two tectonic-magma areas of Wuyishan and south-west Jiangxi.
依据不同构造岩浆区单元 ，江西中南部中新元古代 -晚三叠世的侵入岩可划分为武夷山构造岩浆区、赣西南构造岩浆区。
It is suggested that Cerambycidae may originate at least before breakup of Pang-aea in Middle Triassic;
结果表明，天牛科的起源至少应追溯到三叠纪中期联合古陆分离之前；
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