Based on isostasy principle, this paper made out a correction method for the calculation of disconformity erosion amount.

考虑地壳均衡效应，可以对传统的地层剥量计算方法进一步修正。

Denuded by the Indochina movement, the core of the palaeohigh has no cap rocks like the J4 gyprock.

古隆起核部因曾遭受早印强烈的剥，已无嘉四段良好的石膏作盖层。

The upthrow-side of the fault is eroded and the downthrow-side have a series of fan systems.The fan system is a good ...

断裂上升盘遭剥,下降盘发育一系列扇体,为油气聚集的有利场所。

The sandstones of the Turpan Basin belong mostly to graywacke and their compositional and textural maturity are generally low,indicating a strong erosional and rapid transportational environment.

吐-哈盆地的砂属杂砂类，总的结构成熟度和成分成熟度均较低，形成于强烈剥、快速搬的沉积环境中。

Based on isostasy principle, this paper made out a correction method for the calculation of disconformity erosion amount.

虑地壳均衡效应，可对传统的地层剥量计算方法进一步修正。

Denuded by the Indochina movement, the core of the palaeohigh has no cap rocks like the J4 gyprock.

古隆起核部因曾遭受早印支运动强烈的剥，已无嘉四段良好的石膏岩作盖层。

The upthrow-side of the fault is eroded and the downthrow-side have a series of fan systems.The fan system is a good ...

断裂上升盘遭剥,下降盘发育一系列扇体,为油气聚集的有利场所。

The sandstones of the Turpan Basin belong mostly to graywacke and their compositional and textural maturity are generally low,indicating a strong erosional and rapid transportational environment.

吐-哈盆地的砂岩主要属杂砂岩类，总的结构成熟度和成分成熟度均较低，形成于强烈剥、快速搬运的沉积环境中。

Based on isostasy principle, this paper made out a correction method for the calculation of disconformity erosion amount.

考虑地壳均衡效应，可以对传统的地层量计算方法进一步修正。

Denuded by the Indochina movement, the core of the palaeohigh has no cap rocks like the J4 gyprock.

古隆起核部因曾受早印支运动强烈的，已无嘉四段良好的石膏岩作盖层。

The upthrow-side of the fault is eroded and the downthrow-side have a series of fan systems.The fan system is a good ...

断裂上升,发育一系列扇体,为油气聚集的有利场所。

The sandstones of the Turpan Basin belong mostly to graywacke and their compositional and textural maturity are generally low,indicating a strong erosional and rapid transportational environment.

吐-哈盆地的砂岩主要属杂砂岩类，总的结构成熟度和成分成熟度均较低，形成于强烈、快速搬运的沉积环境中。

Based on isostasy principle, this paper made out a correction method for the calculation of disconformity erosion amount.

考虑地壳衡效应，可以对传统的地层剥量计法进一步修正。

Denuded by the Indochina movement, the core of the palaeohigh has no cap rocks like the J4 gyprock.

古隆起核部因曾遭受早印支运动强烈的剥，已无嘉四段良好的石膏岩作盖层。

The upthrow-side of the fault is eroded and the downthrow-side have a series of fan systems.The fan system is a good ...

断裂上升盘遭剥,下降盘发育一系列扇体,为油气聚集的有利场所。

The sandstones of the Turpan Basin belong mostly to graywacke and their compositional and textural maturity are generally low,indicating a strong erosional and rapid transportational environment.

吐-哈盆地的砂岩主要属杂砂岩类，总的结构成和成分成较低，形成于强烈剥、快速搬运的沉积环境中。

Based on isostasy principle, this paper made out a correction method for the calculation of disconformity erosion amount.

考虑地壳应，可以对传统地层剥量计算方法进一步修正。

Denuded by the Indochina movement, the core of the palaeohigh has no cap rocks like the J4 gyprock.

古隆起核部因曾遭受早印支运动强烈剥，已无嘉四段良好石膏岩作盖层。

The upthrow-side of the fault is eroded and the downthrow-side have a series of fan systems.The fan system is a good ...

断裂上升盘遭剥,下降盘发育一系列扇体,为油气聚集有利场所。

The sandstones of the Turpan Basin belong mostly to graywacke and their compositional and textural maturity are generally low,indicating a strong erosional and rapid transportational environment.

吐-哈盆地砂岩主要属杂砂岩类，总结构成熟度和成分成熟度较低，形成于强烈剥、快速搬运环境中。

Based on isostasy principle, this paper made out a correction method for the calculation of disconformity erosion amount.

考虑地壳均衡效应，可对传统的地层剥量计算方法进一步修正。

Denuded by the Indochina movement, the core of the palaeohigh has no cap rocks like the J4 gyprock.

古隆起核部因曾遭受早印支运动强烈的剥，已无嘉四段良好的石膏岩作盖层。

The upthrow-side of the fault is eroded and the downthrow-side have a series of fan systems.The fan system is a good ...

断裂升盘遭剥,下降盘发育一系列扇体,为油气聚集的有利场所。

The sandstones of the Turpan Basin belong mostly to graywacke and their compositional and textural maturity are generally low,indicating a strong erosional and rapid transportational environment.

吐-哈盆地的砂岩主要属杂砂岩类，总的结构成熟度和成分成熟度均较低，形成于强烈剥、快速搬运的沉积环境中。

Based on isostasy principle, this paper made out a correction method for the calculation of disconformity erosion amount.

考虑地壳均衡效应，可以对传统的地层剥量计算方法进一步修正。

Denuded by the Indochina movement, the core of the palaeohigh has no cap rocks like the J4 gyprock.

古隆起核部因曾遭受早印支运动强烈的剥，四段良好的石膏岩作盖层。

The upthrow-side of the fault is eroded and the downthrow-side have a series of fan systems.The fan system is a good ...

断裂上升盘遭剥,下降盘发育一系列扇体,为油气聚集的有利所。

The sandstones of the Turpan Basin belong mostly to graywacke and their compositional and textural maturity are generally low,indicating a strong erosional and rapid transportational environment.

-哈盆地的砂岩主要属杂砂岩类，总的结构成熟度和成分成熟度均较低，形成于强烈剥、快速搬运的沉积环境中。

Based on isostasy principle, this paper made out a correction method for the calculation of disconformity erosion amount.

考虑地壳均衡效应，可以对传统的地层剥量计算方法进一步。

Denuded by the Indochina movement, the core of the palaeohigh has no cap rocks like the J4 gyprock.

隆起核部因曾遭受早印支运动强烈的剥，已无嘉四段良好的石膏岩作盖层。

The upthrow-side of the fault is eroded and the downthrow-side have a series of fan systems.The fan system is a good ...

断裂上升盘遭剥,下降盘发育一系列扇体,为油气聚集的有利场所。

The sandstones of the Turpan Basin belong mostly to graywacke and their compositional and textural maturity are generally low,indicating a strong erosional and rapid transportational environment.

吐-哈盆地的砂岩主要属杂砂岩类，总的结构成成分成均较低，形成于强烈剥、快速搬运的沉积环境中。

Based on isostasy principle, this paper made out a correction method for the calculation of disconformity erosion amount.

考虑壳均衡效应，可以对传层量计算方法进一步修正。

Denuded by the Indochina movement, the core of the palaeohigh has no cap rocks like the J4 gyprock.

古隆起核部因曾遭受早印支运动，已无嘉四段良好石膏岩作盖层。

The upthrow-side of the fault is eroded and the downthrow-side have a series of fan systems.The fan system is a good ...

断裂上升盘遭,下降盘发育一系列扇体,为油气聚集有利场所。

The sandstones of the Turpan Basin belong mostly to graywacke and their compositional and textural maturity are generally low,indicating a strong erosional and rapid transportational environment.

吐-哈盆砂岩主要属杂砂岩类，总结构成熟度和成分成熟度均较低，形成于、快速搬运沉积环境中。