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湖相层序地层学
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  lacustrine sequence stratigraphy
     In this paper, The Lacustrine sequence stratigraphy of the early Tertiary in the Jiyang depression is systematically studied on the basis of geological data, well logging data,seismic data ,and so on.
     综合运用岩心资料、测井资料、地震资料,对济阳坳陷下第三系湖相层序地层学进行了系统研究。
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  “湖相层序地层学”译为未确定词的双语例句
     In lecustrine sequence stratigraphy,the retrogradation reflection represents transgrassive system tract with condensed section as its cap,which is overlaid by high-stand system tract with progradation reflection or parallel reflection.
     在湖相层序地层学中 ,具退积反射地层就是水进体系域 ,顶界即密集段 ,上覆为具前积反射或平行反射的高位体系域。
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  相似匹配句对
     and lacustrine facies is distributed relatively wide .
     分布则较为广泛。
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     Turbidity current deposits of lake facies in northwestern China
     西北地区浊流沉积
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     Thousand-Islet Lake
     千岛
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     The Lake on a Plateau
     高原的
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     PHASE AND ITS SIGNIFICANCE
     的涵义
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Retrogradation reflection is a reflected phenomenon that reflects the thinning strata and truncated its top in toward basin center,which is different from that takes place generally in basin margin.The retrogradation reflection is rarely seen in continental basin and usually takes place in lacustrine deposition only when accomodation space greatly increases due to quick rise of lake level for a long period or gradual reducing and retreat of main solitary source supply from depression center.The retrogradation...

Retrogradation reflection is a reflected phenomenon that reflects the thinning strata and truncated its top in toward basin center,which is different from that takes place generally in basin margin.The retrogradation reflection is rarely seen in continental basin and usually takes place in lacustrine deposition only when accomodation space greatly increases due to quick rise of lake level for a long period or gradual reducing and retreat of main solitary source supply from depression center.The retrogradation direction usually points to the main source supply direction.In lecustrine sequence stratigraphy,the retrogradation reflection represents transgrassive system tract with condensed section as its cap,which is overlaid by high-stand system tract with progradation reflection or parallel reflection.The transgrassive system tract with retrogradation reflection often happens in a fair large order cycle (4~10 Ma) of lake level rise-and-fall.

退积反射是地层厚度向凹陷中心减薄且其顶部被“削截”的一种反射现象 ,与一般发生在凹陷边缘地层顶界被削截减薄的情形不同。陆相盆地中退积反射较少见 ,一般仅出现在湖相沉积中 ,而且只有当湖平面快速长期上升和单一主物源碎屑供应逐渐减少后退 ,引起可容空间大幅度增大时才可形成。它的退覆方向一般指示了单一主物源的方向。在湖相层序地层学中 ,具退积反射地层就是水进体系域 ,顶界即密集段 ,上覆为具前积反射或平行反射的高位体系域。具退积反射的水进体系域往往发生在较大级别的湖面升降旋回 (4~ 10 Ma)中。

 
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