此方法在中国南方海相沉积盆地可有较好的应用前景。
This method will have a good applied foreground in marine strata in southern China.
中侏罗统是其盆地发育最全、分布最广泛的海相沉积层系。
Middle Juassic marine sedimentary strata are widespread in the basin.
由此可见，南海盆地中生代海相沉积岩具有较好的勘探潜力。
In summary, Mesozoic seafacies sedimentary rocks in the Ancient South China Sea Basin have a very good exploration potential.
十万山盆地是在印支期海相沉积基底上发育的中新生界陆相沉积盆地。
Shiwanshan basin has a Mesozoic to Cenozoic continental sedimentary cover lies over a basement of marine-facies Indosinian deformation.
织金新华磷矿是我国扬子地台西南缘早寒武世重要的海相沉积磷矿床。
Zhijin Xinhua phosphate deposits is an important Marine sedimentary phosphate deposits formed in Early Cambrian Epoch located in South-west edge of Yangtze Platform.
湖润锰矿床由海相沉积的原生碳酸锰矿床和表生富集的氧化锰矿床组成。
Hurun manganese deposit is consisted of Marine sedimentary primary manganese carbonate ores and supergene enrichment oxide ores.
东海盆地周边地质表明存在有中生代、古生代地层，并有过海相沉积环境。
The geology of the surrounding areas of east China sea basin indicates that Marine environment: existed during middle-late Mesozoic era and late Palaecz - oic era.
稀土组成模式及稀土元素配分模式图表明是较典型的海相沉积物稀土配分模式。
The composition mode of REE and distribution mode of REE show that this mode of distribution of REE is typical Marine deposit and belongs to genesis of Marine deposit.
海绿石是海相沉积的指相矿物，通常形成于海进系列，与低的沉积物供应速率有关。
Glauconite as a typical facies mineral is generally regarded as accompanied with transgression sequence, with a low sedimentation rate.
陆相沉积环境与海相沉积环境有很大的差异，相应的可容空间及层序演化控制因素也不同。
There are many differences between terrestrial and marine environment with different controlling factors of corresponding containable space and the sequence evolution.
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.
晚渐新世—中中新世，盆地逐渐由断陷转为断拗，沉积范围不断扩大，整体处于海相沉积环境。
During the period from Late Oligocene to Middle Miocene, the basin changed from rifting to depression, and the depositional area continued to expand in the Marine environment.
一般为玄武岩、页岩发育的土壤可提取态钛含量高于花岗岩、砂岩、浅海相沉积物发育的土壤；
In general, contents of extractable Ti of soils from basalt and shale are higher than those from granite, sandstone, and shallow sea deposits;
三叠纪末的印支运动结束了柴达木地块及其周缘地区的海相沉积史，使柴达木地区进入陆内盆地发育新时期。
At the end of Triassic period, the Marine sedimentation on Qaidam Massif (including its surroundings) has ended, and interior basin started to develop in Qaidam area.
利用自行改装后的三轴蠕变仪对海相沉积的营口软土进行蠕变试验，获得了在不同围压、不同偏应力条件下的剪切应变与时间关系数据。
The relationship between shear strain and time of Yingkou soft soil is obtained under a series of different cell pressures and different deviator stresses.
利用自行改装后的三轴蠕变仪对海相沉积的营口软土进行蠕变试验，获得了在不同围压、不同偏应力条件下的剪切应变与时间关系数据。
The relationship between shear strain and time of Yingkou soft soil is obtained under a series of different cell pressures and different deviator stresses.
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