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、不同类型油气了运聚成条件，为油气多源复合成了前。

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...

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、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，又为同时代、同类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代发育起来的断-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、不同类型气提供了运聚成藏条件，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...

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，又为不同时、不同类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发育起来的断-坳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...

构造运动，又为不同时代生烃、不同类型油气提供了运聚条件，为油气源复提供了前提。

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.

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。