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1)  Erosion Thickness Restoration
剥蚀厚度恢复
1.
Study the Erosion Thickness Restoration of Qianjiang Formation in Qianjiang Depression;
潜江凹陷潜江组地层剥蚀厚度恢复研究
2)  Eroded Thickness Restoration
剥蚀恢复
3)  denudation thickness
剥蚀厚度
1.
Many methods can be used to restore formation denudation thickness, such as stratigraphic correlation, deposition velocity, well log, compaction curve, vitrinite reflectance, sporopollen and wave analysis method, etc.
地层剥蚀厚度恢复的方法有很多种,例如地层对比法、沉积速率法、测井曲线法、压实曲线法、镜质体反射率法、孢粉法及波动分析法等。
2.
It is an important basis for reconstructing the strata denudation thickness in basin quantitative study.
恢复地层剥蚀厚度是对盆地进行定量研究的重要基础工作。
3.
Strata antithesis method uses two dimension seismic data to comeback the plane distribution character of Xishanyao Formation,and sedimentary ratio analysis method uses well geological layer and precise chronology framework data to comeback well denudation thickness.
综合利用地层对比法和沉积速率法估算了准噶尔盆地西山窑组剥蚀厚度,用全盆地34条二维区域地震测线资料,估算了西山窑组剥蚀厚度的平面分布特征。
4)  eroded strata thickness
剥蚀厚度
1.
Restoration of eroded strata thickness in Cretaceous/Jurassic unconformity in hinterland of Junggar Basin;
准噶尔盆地腹部白垩系/侏罗系不整合地层剥蚀厚度的恢复方法
2.
On the basis of the scientific definition of eroded thickness and the analysis of factors that affect eroded strata thickness, a new category scheme on eroded strata thickness restoration in sedimentary basins is propose.
地层剥蚀厚度的准确恢复对正确重建沉积盆地原始沉积—构造演化史、热史及油气生、排、运、聚史和定量评价油气资源潜力至关重要。
3.
This is the first time to obtain the eroded strata thickness of the fourth member of the Shahejie Formation in Huimin Depression,Bohai Bay Basin system atically by means of vitrinite reflectance.
Dow在1977年提出的利用上下构造层镜质体反射率(Ro)差值来估算不整合面地层剥蚀厚度的方法,在国内仍有广泛的应用。
5)  erosion thickness
剥蚀厚度
1.
Restoration of erosion thickness in Xuanhan-Daxian area,northeastern Sichuan basin;
川东北宣汉—达县地区地层剥蚀厚度恢复
2.
The cause of "shallow maturation" of source rock in Jinhu depression is analyzed with data of source rock maturity index and palaeotemperature test on the basis of reconstruction of erosion thickness of Sanduo formation and analysis of thermal evolution history.
从烃源岩成熟度指标、古温标测试数据等出发,在三垛组地层剥蚀厚度恢复和热演化史分析的基础上,对金湖凹陷烃源岩"浅熟"原因进行了初步探讨。
3.
Using seismic, logging, and assaying data, and combined with vitrinite reflectance erosion thickness restoration method and seismic stratigraphy Paleogeomorphology restoration way, we have restored Caledonian paleogeomorphology in the central area of Tarim.
利用地震、测井和分析测试资料,结合镜质体反射率剥蚀厚度恢复法和地震地层学古地貌恢复法,对塔中地区中加里东期古地貌进行了恢复。
6)  Eroded thickness
剥蚀厚度
1.
According to this method,the eroded thickness of strata of Turpan and Hami basin can be obtained as follows:the Triassic is less than 500m in the southern area of basin;the Jurassic is between 600m and no erosion in Taibei depression in the northern area of basin;and is from 800m to 1800m in the foreland mountains of Taibei depression.
以吐-哈油田为例,用镜质体反射率和磷灰石裂变径迹方法综合求取了地层剥蚀厚度。
补充资料:剥蚀面
剥蚀面
plane of denudation

   见夷平面。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条