凹陷中新生代火山作用强烈，也具有多期性。
The volcanism is strong in Cenozoic and has several periods.
中新生代盆地；古气候演化；砂岩型铀矿；
Meso-Cenozoic basin; paleo-climate evolution; sandstone type uranium deposit;
豫皖交界地段中新生代盆地位于合肥盆地的南缘。
The Meso Cenozoic basin in Anhui Henan border area is located in the south of Hefei basin.
辽宁省中新生代盆地地层中赋有有丰富的地热资源。
Rich geothermal resources are hosted in the Meso-Cenozoic basins in Liaoning Province.
榆中盆地位于兰州—定西中新生代凹陷盆地的中部。
Yuzhong Basin is located in the middle part of Lanzhou Dingxi Mesozoic Cenozoic depression.
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.
从海参1井钻井剖面出发，建立六盘山盆地中新生代层序地层格架。
Starting from the profile of Haishen no. 1 well, this paper establishes the sequential stratigraphic framework of middle Cenozoic in Liupanshan Basin.
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.
柴达木盆地形成于中新生代，是我国西北地区主要的含油气盆地之一。
Qaidamu basin is one of the most impotent oil and gas bearing basins in China northwestward.
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu Tancheng?
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu (TanchengLujiang) fault zone.
具有工业意义的油气田均位于构造隐性急变带与中新生代盆地的立交地段。
The most of oil fields with industrial index are also located at the cross districts between basin and tectonic recessive geochemical boundaries.
泌阳凹陷是一个中新生代断陷盆地，岩性变化快，断裂发育，油藏类型多。
Miyang Depression is a Mesozoic-Cenozoic fault basin, where lithologic change is fast, fault is developed, reservoir type is various.
南襄盆地是中新生代含油气沉积盆地，它们形成演化与断裂活动密切相关。
Nanxiang basin is a Mesozonic and Cenozonic Era deposit basin which contains oil and gas, its formation and evolution has close relation to faults activity.
都日木断陷为二连盆地的中新生代单断型凹陷，其地表为腾格尔沙漠的一部分。
Durimu faulted depression is a Cenozoic simple fault type depression in Erlian basin. Its surface is a part of Tengger Desert.
特提斯成矿域仅出露于青海的南部，三江成矿区的北段以中新生代成矿为特点。
The Tethyan metallogenic domain consists mainly of north Sanjiang metallogenic belt located in southeast Qinghai-Tibet plateau, with middle Cenozoic being the major metallogenic period.
将中新生代深成侵入岩划分为拉轨岗日花岗岩带和冈底斯花岗岩带两个岩浆带；
The Mesozoic and Cenozoic plutonic intrusive rocks are grouped into the Lhagoi Kangri and Gangdise granite zones.
滇西兰坪盆地是一个重要的中新生代陆相盆地，产有丰富的铅锌铜银矿产资源。
The Lanping basin in west Yunnan, China, is an important Meso-Cenozoic continental facies basin, which is an abundant mineral resource of Pb, Zn, Cu, Ag, and so on.
山西高原内部中新生代拆离构造特征与太行山前类似，伸展构造以拉分断陷为主。
The extensional structures in Mesozoic-Cenozoic inside the Shanxi Plateau are mainly characteristic of pull-apart basin development, similar to the ones in front of the Taihang Mountains.
松辽盆地地处中国东北部是中新生代形成的大型陆相盆地，是我国重要的石油产区。
Songliao basin is a large scale land basin of Meso-cenozoic at northeast of China, which is one of the most important oil-producing area.
川东北地区是上扬子板块北缘的中新生代含油气盆地，具有复杂的构造和成藏历史。
Northeast Sichuan basin is a Mesozoic-Cenozoic basin in north margin of the Yangtse plate, which has a complex tectonic background and hydrocarbon accumulation history.
中国及邻区中新生代大型大陆扩张盆地的特点和性质取决于距离相邻相关大洋的位置。
Characteristics and nature of the Meso-Cenozoic great continental spreading basins in China and adjacent regions depend on the relative positions of the allied adjacent oceans.
重点讨论了中国西部中新生代大型沉积盆地变形构造的几何结构样式、形成与演化模式。
This paper discusses the geometrical style, formation and evolution of deformed structures in the large scale Meso Cenozoic sedimentary basins in the west of China.
花海凹陷是一个小型的中新生代沉积断陷，其油气成藏条件在中小型盆地中具有代表性。
Huahai sag is a small sedimentary fault-depression basin formed during Mesozoic-Cenozoic periods, its accumulation conditions of oil and gas represent the characteristics of medium-small basins.
都日木断陷是二连盆地中一个中新生代单断型凹陷，其地表景观为腾格尔沙漠的一部分。
Durimu sag is a Mesozoic Cenozoic sag of Erlian Basin and its landscape is a part of Tengger Desert.
南华北中南部中新生代盆地的形成演化主要受郯庐断裂带、大别造山带构造运动的制约。
The formation and evolution of the Meso-Cenozoic basins in the middle and southern part of southern North China was mainly controlled by the Tanlu fault system and the Dabie orogenic belt.
在华北地台北缘中新生代火山岩发育区，发现大型铀钼矿床，其外围被第四系广泛覆盖。
A large U-Mo deposit was found on the northern margin of north China Platform, where the Mesozoic and Cenozoic volcanics are developed. This area is widely covered by the Quaternary sediments.
伊朗盆地是在中新生代受古特提斯洋与新特提斯洋的扩张闭合控制下形成的被动大陆盆地。
The Iran basin is a passive continental basin formed in Meso-Cenozoic under the control of the extensional closing of Paleotethys and Neo-tethys oceans.
川东北地区是一个具有复杂构造的中新生代盆地，以海相沉积为主的三叠系是重要的储层。
Abstract1 Northeast Sichuan basin is a Mesozoic-Cenozoic basin with complex tectonics, Triassic formation based on Marine deposits was an important potential resource and reservoir.
川东北地区是一个具有复杂构造的中新生代盆地，以海相沉积为主的三叠系是重要的储层。
Abstract1 Northeast Sichuan basin is a Mesozoic-Cenozoic basin with complex tectonics, Triassic formation based on Marine deposits was an important potential resource and reservoir.
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