陆相断陷盆地具有特定的沉积环境。
Continental faulted basins formed in specific depositional environment.
在伸展断陷盆地内均有明显的沉积响应。
There were obvious depositional response in the extensional faulted basin.
西峡恐龙遗址属于白垩纪断陷盆地沉积。
Xixia ruins belong to the Cretaceous period dinosaur rift sedimentary basin.
东亢矿泉水处于临汾断陷盆地边缘山前地带。
Dongkang mineral water is Located at the edge of Linfen faulted basins.
断陷盆地特有的构造格架，使油气按带分布。
The characteristic geotectonic framework of many depression-faulted bas - ins, made the hydrocarbon distributed as belts.
发育同沉积构造坡折带是断陷盆地的基本特征。
Syndepositional structural slope-break zone is a basic characteristic of rift-subsidence basin.
就构造意义而言，火山带实质上是断陷盆地带。
In fact, the volcanic rock zone is a fault subsidence basin zone in tectonic sense.
陡坡构造带是不对称断陷盆地重要的构造单元。
Abrupt slope structure belt was one of the important structure units for asymmetric fault basin.
火山断陷盆地是构造-岩浆-地热体系的最活跃场所。
The volcano-graben basins are the most active fields for the tectonic-magmatic-geothermal system.
山西太原盆地是我国北方典型的大型新生代断陷盆地。
Taiyuan basin is a representative large-scale Cenozoic rift basin in Shanxi Province, northern China.
小型断块圈闭是陆相断陷盆地最重要的圈闭类型之一。
Small fault trap is one of the important trap types in continental fault basin.
德兴盆地大体上是一个岩层向北倾斜的单斜式断陷盆地。
Dexing Basin is generally a monocline downfaulted one with north-dipping rock format ion.
昆明南市区软土是内陆断陷盆地型软土的一个典型代表。
The soft soil in South city of Kunming is a typical internal continental type soft soil.
胶州湾为一断陷盆地，棋盘格式构造起着主要控制作用。
Jiaozhou Bay is a fault basin and the chess board structure has played the main control role in its formation.
海拉尔盆地是在华力西褶皱基底上形成的中生代断陷盆地。
Hailar basin is a fault-depressed basin formed on Variscan folded basement.
陆相断陷盆地中，地层水中离子的运移、聚集过程比较复杂。
The process of migration and accumulation of ions in formation water was very complex in continental down-faulted basin.
不同类型的扇三角洲沉积可发育在断陷盆地演化的不同阶段。
Various types of fan delta systems have been developed in different evolution stages of faulted basin.
下部的火山断陷盆地和上覆的沉积坳陷盆地组成了二元结构的盆地。
The underlying volcanic fault basin combines with the overlying downwarped basin to form a basin with a binary structure.
汪清县东北部中生代火山断陷盆地火山岩中夹一套含煤碎屑岩地层。
The Mesozoic volcanic rocks are interbedded with a series of coal-bearing clastics in the faulted basin in the northeastern part of Wangqing County.
晚侏罗纪—早白垩世为拉张断陷盆地，第三纪以来为挤压坳陷盆地。
It was rift basin in Late Jurassic Early Creaceous and squeezed sag basin since Cenozoic.
辽西地区的早侏罗世—早白垩世盆地群是一类颇具特色的断陷盆地群。
Early Jurassic to early cretaceous basin group of western Liaoning is a distinguished group of fault basin.
早期由边缘断陷转化为大型断陷盆地，至上新世湖水淹没了大部地区；
The marginal fault-depression was transformed into a large basin, most of which were drowned by lake water in Pliocene.
济阳断陷盆地不同区带油气运移的控制因素、输导体系和运聚方向各异。
In Jiyang rifted-basin, there are different factors to control hydrocarbon migration, carrier systems and migration-accumulation directions in various zones.
东营断陷盆地古近系发育的地层流体超压系统对油气运聚、成藏至关重要。
The formation superpressure system developed in the Palaeogene system of Dongying Fault Basin plays an important role in hydrocarbon migration and accumulation.
柴西南隆升导致中侏罗世地层向北、北东迁移，并出现反向箕状断陷盆地。
Uplift in the southwestern Qaidam Basin led to the migration of Middle Jurassic strata to the north and west, and resulted in the formation of inverted haft-graben fault basin.
文山盆地属于岩溶断陷盆地，研究区基岩主要为碳酸盐岩、粘土岩与碎屑岩。
The Wenshan basin is karst faulted basin, the main rock is carbonate, clay and clastic.
断裂是断陷盆地的一种普遍地质构造现象，因此，研究断裂的规律性十分重要。
The faults is common geologic structural phenomenon in faulted basin, therefore, studying the rule of faults is of great importance.
伊通地堑是一个主体在海西期褶皱基底上发育起来的第三纪含油气走滑断陷盆地。
The Yitong Graben is a Tertiary petroliferous strike-slip fault basin developed on the Hercynian fold basement.
湖盆层序属于新立城断陷盆地的发育早期，冲积层序属于新立城盆地的发育晚期。
The lake basin sequence occurred in lake basin belonging to early stage of Xinlicheng basin's development and the alluvial sequence occurred in river basin belonging to later stage of that.
内蒙古大青山及其毗邻的呼和浩特断陷盆地是研究剥蚀和地壳均衡隆起的理想地区。
The Daqingshan Mountains and its adjacent Huhehot fault basin, Nei Monggol, are the ideal area to study denudation and uplift.
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