陆相沉积 meaning in Chinese
continental deposits
continental sedimentation
continentaldeposits
continentalsediment
land sediment
nonmarine deposit
terrestrial deposits
Examples
- For a long time , the above division of systems tracts has been a classical model in the study of continental deposition
长期以来，从国外传入的三个水位域沉积体系划分成为研究陆相沉积的经典模式。 - Terrestrial sediments can be found in shengli oil filed beginning from permian to tertiary . in addition , source beds are widely distributed
胜利油区从古生代二迭纪到新生代第三纪每个地质时期都有陆相沉积，也广泛地发育着生油层。 - The terrestrial sediments reservoirs are complexity and diversify , they are very important for reservoir evaluation , that districting bed boundary properly and stating the truthful resistivity of reservoir
由于陆相沉积储层的复杂性、多样性，准确划分地层界面，确定储层的真电阻率，对储层的评价是至关重要的。 - Lowstand system tract , transgressive system tract and highstand system tract are all have characteristic of changing gradually in tune and space . it ' s the new theory of sequence stratigraphy applying on the continental sedimentary basin
低水位、水进及高水位体系域都具有时间、空间渐变的特征，这是层序地层学理论应用于陆相沉积盆地的新认识。 - Conclusion are obtained as follows : 1 . basin accepted sedimentation since sinian , and strata were well developed . it was marine sedimentary series from sinian to middle - triassic and become continental sedimentary series since late - triassic
主要成果及认识如下： 1 、盆地自震旦纪以来长期接受沉积，地层发育良好，震旦纪至中三叠世为海相沉积体系，晚三叠世以后为陆相沉积体系。