通过对东大滩—东温泉地区的路线地质观测与构造填图，在东昆仑南部发现晚新生代大型逆冲推覆构造系统。
A large-scale Late Cenozoic overthrust system has been found in the southern East Kunlun Mountains through tectonic mapping and geological reconnaissance in the Dongdatan-East Wenquan area.
长江流域的地质-生态环境与自然灾害受到中新生代以来地壳运动和秦岭-大别等造山作用的严格制约与影响。
Natural disasters and eco-environment in the Yangtze Valley have been restricted and impressed by crustal movement and Qinling-Dabie orogenesis since the Mesozoic and Cenozoic.
根据胶莱盆地区域地质特征，地球动力学背景及盆地中、新生代沉积特征分析，论述盆地的发育和演化阶段，并对胶莱盆地含油气前景进行探讨。
The evolution features of the Jiaolai Basin are discussed in this paper on the basis of its regional structure, geodynamic background and sedimentary features of the Mesozoic and Cenozoic.
本文对晚新生代贵州喀斯特地貌演进的三大控制因素 ，即地质基础、新构造运动及挽近气候波动进行了分析论证。
In this paper, three determined factors influencing on the evolution of karst geomorphology of upper Cenozoic in Guizhou, e.
楚雄盆地是我国南方具有良好石油地质条件的大中型中-新生代改造型含油气盆地的一个典型代表。
Chuxiong basin is a typical reformed basin, which formed during Mesozoic-Cenozoic periods in south of China and has good petroleum geological condition.
下面所列举的是分布于分流和三角洲前绿砂体的油气田的例子，在地质时代上从晚古生代至中新生代。
The following examples of oil and gas fields in distributary and delta- fringe sand bodies range in age from late paleozoic to middle cenozoic.
唐古拉山地区广泛出露早新生代陆相地层，较好地记录了青藏高原北部新生代地质构造演化与古环境变迁的过程。
The Cenozoic fluvial strata, exposed widely in the Tanggula Mountains, detaily recorded the information of the uplift of the northern Tibet Plateau and the paleoenvironmental evolution.
结合野外地面地质调查成果，并通过对地震、大地电磁等地球物理资料的精细解释构建了塔里木盆地东南缘新生代断裂系统。
Combined with the field geologic investigation, and the detailed interpretation of seismic, MT and other geophysical information, the fault system has been constructed in the southeastern Tarim basin.
记录中国北方晚新生代以来地球演化、生物进化与古人类活动的“泥河湾层” ，是珍贵的地质遗迹。
According to the records of early human activities, Nihewan strata is an invaluable geological relic that has undergone the evolution of the earth and creations since the later Cenozoic Era.
中新生代是地质历史中海水锶同位素组成变化最大的时期。
The Mesozoic and the Cenozoic are geological periods in which the greatest change in the composition of seawater strontium isotopes occurred.
青藏高原新生代以来的持续性、阶段性隆升是地球演化过程中重要的地质和环境事件。
The continuous and periodic uplift of the Qinghai-Tibet Plateau since the Cenozoic is an important geological and environmental event during the evolution of the Earth.
通过共和盆地西北部晚新生代地层的野外地质调查，发现上新世地层中存在一期角度不整合面。
An angular unconformity within the Pliocene stratum was found during field exploration in northwestern part of the Gonghe Basin.
金矿形成于新生代第三纪古新世和始新世初的陆内拉张地质构造环境中。
The gold mineralization in the Boka-Tuobuka area took place in Paleocene and early Eocene, intra-continental extensional geotectonic environment.
从上个世纪初开始，国内外学者就这一地区中新生代的地质与构造问题开展了大量的研究工作，取得了许多重要的认识。
From the beginning of the last century, many researchers have been focused on the Mesozoic stratigraphy and tectonics in this area and much progress was done and achieved.
中国北方连续堆积的晚新生代风成红粘土-黄土，是气候干湿变化的良好地质记录。
There occur thick wind-blown silt deposits which are regarded as a good geological archive of paleoclimatic changes in Late Cenozoic in North China and the central Asia.
中国北方连续堆积的晚新生代风成红粘土-黄土，是气候干湿变化的良好地质记录。
There occur thick wind-blown silt deposits which are regarded as a good geological archive of paleoclimatic changes in Late Cenozoic in North China and the central Asia.
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