The process of successive subsidence or interruptly polystage subsidence existed during the formation of petroleum bearing downwarping regio...

多期构造动，又为不同时代烃、不同类型油气提供成藏条件，为油气多源复合成藏提供前提。

Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.

白音干凹陷为兴蒙海西期多旋回、软碰撞褶皱基底上代发育起来的断-坳型裂谷盆地的次级构造单元。

The process of successive subsidence or interruptly polystage subsidence existed during the formation of petroleum bearing downwarping regio...

多期构造运动，又为不同时代生烃、不同类型油气提供了运聚成藏条件，为油气多源复合成藏提供了前提。

Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.

白音干凹陷为兴蒙海西期多旋回、软碰撞褶皱基底上晚中生代发育起来的断-坳型裂谷盆地的次级构造单元。

The process of successive subsidence or interruptly polystage subsidence existed during the formation of petroleum bearing downwarping regio...

多期构造运动，又为不同时代生烃、不同类型油气提供了运聚成藏条件，为油气多源复合成藏提供了前提。

Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.

白音干凹陷为兴蒙海西期多旋回、软碰撞褶皱基底上晚中生代发育起来的断-坳型裂谷盆地的次级构造单元。

The process of successive subsidence or interruptly polystage subsidence existed during the formation of petroleum bearing downwarping regio...

多期构造运动，又为不同时生烃、不同类型油了运聚成藏条件，为油多源复合成藏了前。

Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.

白音干凹陷为兴蒙海西期多旋回、软碰撞褶皱基底上晚中生起来的断-坳型裂谷盆地的次级构造单元。

The process of successive subsidence or interruptly polystage subsidence existed during the formation of petroleum bearing downwarping regio...

期构造运动，又为不同时代生烃、不同类型油气提供了运聚成藏条件，为油气源复合成藏提供了前提。

Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.

白音干凹陷为兴蒙海西期旋回、软碰撞褶皱基底晚中生代发育起来的断-坳型裂谷盆地的次级构造单元。

The process of successive subsidence or interruptly polystage subsidence existed during the formation of petroleum bearing downwarping regio...

多期构造运动，又不同时代生烃、不同类型油气供了运聚成藏条件，油气多源复合成藏供了。

Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.

音干兴蒙海西期多旋回、软碰撞褶皱基底上晚中生代发育起来的断-坳型裂谷盆地的次级构造单元。

The process of successive subsidence or interruptly polystage subsidence existed during the formation of petroleum bearing downwarping regio...

多期构造运动，又为不同时代生烃、不同类型油气提供了运聚成藏条件，为油气多源复合成藏提供了前提。

Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.

白音干凹陷为兴蒙海西期多旋回、软碰撞褶皱基底上晚中生代发育起来的断-坳型裂谷盆地的次级构造单元。

The process of successive subsidence or interruptly polystage subsidence existed during the formation of petroleum bearing downwarping regio...

多期构造运动，又为不同时代生烃、不同类型油气提供了运聚件，为油气多源复合提供了前提。

Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.

白音干凹陷为兴蒙海西期多旋回、软碰撞褶皱晚中生代发育起来的断-坳型裂谷盆地的次级构造单元。

The process of successive subsidence or interruptly polystage subsidence existed during the formation of petroleum bearing downwarping regio...

多期造运，不同时代生烃、不同类型油气提供了运聚成藏条件，油气多源复合成藏提供了前提。

Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.

白音干凹陷兴蒙海西期多旋回、软碰撞褶皱基底上晚中生代发育起来的断-坳型裂谷盆地的造单元。