红、赭、粉等颜色来自三叠纪干燥期缓慢形成的沉积物，在足够长的时间里，侵蚀与氧化作用创造出这种奇迹。
The reds, ochres and pinks hail from the much slower deposition during the Triassic's dryer periods, when erosion and oxidation had time to work their magic.
二叠纪末大灭绝之后，三叠纪初残存期和复苏期生态系研究成为当今热点。
The study of the ecosystems in the survival and recovery time in the Early Triassic following the end-Permian mass extinction becomes a hotspot.
以四川盆地西部上三叠统须家河组的砂岩组分为基础，详细分析该期研究区古地理的演化。
Based on the sandstone compositions analysis of the Upper Triassic Xujiahe Formation in Western Sichuan Basin, the authors tried to discuss the paleogeographic evolution of the study area.
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 area of western Sichuan was situated in the southwestern part of an evaporative sea basin (Weixi area) during Leikoupo age in 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。
Nanpan River Basin experienced extension, fault depression in middle-late period of Early Triassic and compression fault rising after Ladinian of Middle Triassic.
四川盆地西部在晚三叠世早期（卡尼期）为被动大陆边缘环境， 沉积岩石单元为马鞍塘组。
The Maantang Formation in western Sichuan basin was probably located in the shelf of the passive continental margin in Upper Triassic.
三叠纪至古近纪，板块挤压作用减弱，准噶尔盆地由强烈压陷期逐渐进入坳陷沉降阶段。
From Triassic to Palaeogene, the plate squeezing action weakened and Junggar basin gradually entered a depression-subsidence phase from the intense compressive phase.
该地区两期主要的成矿作用发生在三叠纪晚期和早侏罗世。
So, this area underwent two main Pb-Zn mineralizing periods, i. e. , late Triassic and early Jurassic.
二叠纪前为地裂运动伊始期； 二纪为地裂运动高峰期；三叠纪为地裂运动衰退期。
Permian, Permian and Triassic were the outset, peak and close stages of the Emei Taphrogenesis, respectively.
两个成藏期分别是三叠纪末和侏罗纪末—白垩纪；
The period of migration and accumulation of oil and gas is Triassic system and from Jurassic system to Cretaceous system.
在巴颜喀拉山群中采获早三叠世和晚三叠世诺利期双壳化石，查明了测区三叠纪巴颜喀拉山群最高层位为诺利期陆棚—海陆交互相沉积。
It is ascertained that the highest horizon of the Triassic Bayan Har Mountain Group in the survey area is Noric shelf-paralic deposits.
主要发育二叠系、三叠系、侏罗系多套烃源岩，燕山运动早期、中—晚期及喜马拉雅运动期为烃源岩的主要生、排烃高峰期。
The periods of early, middle-late Yanshan movement and Himalayan movement are its major periods for hydrocarbon generation and expelling.
晚侏罗世-早白垩世为鄯深构造三叠系油藏的第三个成藏期，现在鄯科1井所产轻质油就是该期注入。
The third stage, lasting from Late Jurassic to Early Cretaceous, has resulted in accumulation of light oil, forming a productivity in Shanke-1.
晚侏罗世-早白垩世为鄯深构造三叠系油藏的第三个成藏期，现在鄯科1井所产轻质油就是该期注入。
The third stage, lasting from Late Jurassic to Early Cretaceous, has resulted in accumulation of light oil, forming a productivity in Shanke-1.
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