The controlling factors and formation mechanism of the continental sequences are important research field in continental sequence stratigraphy.
陆相层序的控制因素与形成机制是陆相层序地层学研究的一项重要内容。
The concept of condensed body, main controlling factors of lacustrine sedimentary sequence, classification of system tracts, and research methods of continental sequence stratigraphy are discussed.
在凝缩体的概念、陆相盆地中湖相沉积层序形成的主控因素、体系域的划分以及陆相层序地层学的研究方法等方面，提出了探讨性的意见。
With the introduction of Sequence Stratigraphy into the study of continental sedimentary basins, some controversial questions arose in our country.
随着陆相沉积盆地研究中层序地层学的引入，在国内引起了一些颇有争议的问题。
Sequence stratigraphy will be encountered with new challenges from continental dynamics of archipelago arc orogenic models and multi mechanism uplifting models.
多岛弧造山模式和多机制的隆升模式等大陆动力学问题也是层序地层所遇到的新挑战。
Finally, the authors look ahead the application potential of sequence stratigraphy to the prospecting for sandstone type uranium deposits in continental depositional basins.
最后，作者展望了层序地层学在陆相沉积盆地内砂岩型铀矿找矿中的应用前景。
The Quaternary of Qaidam basin, being lack of topographic break, was studied based on the theory of sequence stratigraphy, which originated from marine basins in passive continental margin.
依据起源于被动大陆边缘海相盆地的层序地层学基本原理，对缺乏地形坡折的柴达木盆地第四系进行了层序地层研究。
The recognition of sequence boundaries and maximum flooding surfaces is the key problem in the study of sequence stratigraphy of continental strata.
层序界线和最大洪泛面的识别是陆相地层层序地层学研究的关键。
The recognition of sequence boundaries and maximum flooding surfaces is the key problem in the study of sequence stratigraphy of continental strata.
层序界线和最大洪泛面的识别是陆相地层层序地层学研究的关键。
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