博格达山属于晚古生代的陆间裂谷。
秦岭造山带形成于晚古生代至三叠纪。
The Qinling orogenic belt was formed from the Late Paleozoic to the Triassic.
该裂谷为塔里木南缘晚古生代活动带的一部分。
The rift is a part of the late Paleozoic active belt in the margin of Tarim.
粤北晚古生代沉积盆地存在三种类型的矿化流体。
There are three types of mineralization fluid in Later Paleozoic sedimentary basin in North-Guangdong province.
辉绿玢岩是冈瓦纳被动陆缘在晚古生代裂解的产物。
Diabase-porphyrite was the splitting product of passive margin of Gondwana Continent in Late Jurassic.
晚古生代早期的洋盆较狭窄，生存时间为数千万年。
The ocean basin became more narrow in early Late Paleozoic, which last several millions years.
这是最早化石藻类之一，描述了这种从晚古生代岩石作为。
This was one of the first fossil algae to be described as such from Late Paleozoic rocks.
准噶尔盆地是晚古生代以来多期形成的复合叠加前陆盆地。
Zhungaer basin is a composite and superimposed foreland basin since late Paleozoic.
主要发育晚古生代—中生代的地层，尤其是三叠系广泛分布。
The strata are mainly late Paleozoic-Mesozoic with widely distribution of Triassic strata.
湖南省东南部的晚古生代和中生代含煤盆地多处发现推覆构造。
Several nappes have been found in the late Paleozoic and Mesozoic coal-bearing basins in southeastern Hunail.
研究区晚古生代含煤岩系主要形成于陆表海—海岸平原环境中。
In the research area, the coal series in late Palaeozoic era were mainly formed from epeiric sea - coastal plain environment.
海侵成煤和事件成煤是鄂尔多斯盆地晚古生代煤聚积的基本特色。
Transgressive coal forming and coal forming under event are the essential features of Late Palaeozoic coal accumulation in Ordos basin.
此巨型成矿域以发育中、晚元古代及晚古生代成矿作用为其特点。
This metallogenic province is characterized by the Mid-Late Proterozoic and the Late Paleaozoic mineralizations.
它是由晚古生代前陆坳陷和中新生代山前拗陷迭加而成的复合型盆地。
Generally, the basin is a superimposed basin formed by foreland depression of the Late Paleozoic in the lower, and the piedmont depression of the Meso-Cenozoic in the upper.
本文论述了山西大同晚古生代含煤地层的沉积特征及其层序地层学意义。
The authors discuss the depositional characteristics and sequence stratigraphic significance of late Paleozoic coal-bearing strata of the Datong area, Shanxi.
早石炭世白山组火山岩是甘肃北山地区分布最为广泛的晚古生代火山岩。
Volcanic rocks of early Carboniferous Baishan Formation were widely distributed in the Beishan area of Gansu Province.
华北晚古生代煤具有中部和南部变质程度较高而南部边缘和北部低的特点。
In north China, the late Paleozoic coal was metamorphosed mainly to middle and high ranking in the central and southern belts, but only to low, ranking in the northern belt and southern margin.
在晚古生代至早中生代，利文斯顿岛中部处于一个独特的浊积扇的构造环境。
The Central Livingston Island was at a special tectonic setting, fan depositional environment, during Late Palaeozoic Early Mesozoic time.
已知成矿的花岗岩类侵入体主要为中生代岩体，其次为晚古生代华力西期岩体。
The most important metallogenic granitoid intrusions are mainly formed in Mesozoic, secondly late Variscan period.
岩浆活动时期大致为晚古生代早三叠世早期，可能代表古特提斯形成的早期阶段。
The period of magmatic activity is about Late Palaeozoic-Early Triassic, which is probably the early stage of Tethys.
中国早、晚古生代、中生代和新生代成煤期的大地构造性质，在各个地区可有不同。
The tectonic nature of different regions in China in the Early and Late Paleozoic, Mesozoic and Cenozoic coal-forming periods is different.
新疆康古尔金矿床是分布于晚古生代火山岩区受脆韧性剪切带控制的蚀变岩型金矿。
Kangur gold deposit is one of the altered rock types controlled by brittle duc tile shear zone located in Late Paleozoic volcanic rock area.
其成研究区带隶属昆仑成矿省东昆仑前寒武、晚古生代、中生代金铜铅锌铁成矿带。
Metallogenic belt belong to the province of East Kunlun Precambrian, Paleozoic, Mesozoic gold and copper zinc iron ore belt.
北美晚古生代钾盐大规模集中成矿作用，也与该时期北美大陆古赤道位置密切相关。
The extensive deposition of potash salts in North America in Paleozoic Era was associated closely with the position of paleoequator.
驼路沟钴、金矿位于东昆仑褶皱系昆南断褶带内，产于晚古生代二叠系下统石英片岩中。
Tuoluogou cobalt and gold deposit is in the south of the east Kunlun drape. It formed in quartz schist in the forepant Permian of late vecent life.
早古生代时期的喷气喷流型矿床组合和晚古生代—早中生代时期的造山型矿床组合最为重要。
The exhalation-spout type deposits of the early Paleozoic era and the orogenic type deposits of the late Paleozoic to early Mesozoic era are the most important deposit groups.
作者通过对豫西晚古生代煤中微粒体的研究提出了各向异性微粒体，对其次生成因提供了佐证。
The authors suggest that there is a kind of anisotropic micrinite existing in the Late Paleozoic coal seams of western Henan coal field, and the evidences of its secondary origin are provided.
东天山康古尔·塔格金铜矿带位于塔里木板块东北部晚古生代阿齐山—雅满苏火山弧岛带的北缘。
The Kanggultage gold-copper ore belt is located in the northern late Paleozoic Aqishan - Yamansu island arc belt in the northeast of Tarim plate.
在晚古生代岛弧带、弧前海沟带、弧后盆地或陆缘活动带等构造环境下发育有不同的火山岩组合。
Under the tectonic backgrounds of island arc belt, fore - arc trench belt, back - arc basin, and epicontinental active belt of late Paleozoic, it has different volcanic rock characteristics.
华北晚古生代经历了3次大的海平面升降旋回，不同海侵事件在研究区内留下了不同的沉积纪录。
During the Upper Paleozoic in Huabei there were 3 main times of sea level eustacy which caused different deposits in research area.
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