The platform foreslope is composed of the dark grey and celadon calcareous mudstone,siltstone,sandstone intercalated with limestone conglo...

内陆棚以深、绿质泥岩夹浅砂质、质纹层条带为特征,并编制了该区桑塔木组的岩相图。

In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.

该油岩呈深棕褐 ,发育 ,主要由富含有机质纹层和浅钙质纹层形成的毫米级沉积层偶组成。

The platform foreslope is composed of the dark grey and celadon calcareous mudstone,siltstone,sandstone intercalated with limestone conglo...

内陆棚以深灰、灰绿灰质泥岩夹浅灰砂质、灰质纹层条带为特征,并编制了该区桑塔木组的岩理图。

In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.

该油岩呈深灰褐 ,理发育 ,主要由富含有机质纹层和浅灰钙质纹层形成的毫米级沉积层偶组成。

The platform foreslope is composed of the dark grey and celadon calcareous mudstone,siltstone,sandstone intercalated with limestone conglo...

内陆棚以深、绿色质泥岩夹色砂质、质纹层为特征,并编制了该地区桑塔木组的岩相古地理图。

In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.

该油岩呈深色棕褐色 ,理发育 ,主要由富含有机质纹层色钙质纹层形成的毫米级沉积层偶组成。

The platform foreslope is composed of the dark grey and celadon calcareous mudstone,siltstone,sandstone intercalated with limestone conglo...

内陆棚以深、绿色质泥岩夹色砂质、质纹层为特征,并编制了该地区桑塔木组的岩相古地理图。

In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.

该油岩呈深色棕褐色 ,理发育 ,主要由富含有机质纹层色钙质纹层形成的毫米级沉积层偶组成。

The platform foreslope is composed of the dark grey and celadon calcareous mudstone,siltstone,sandstone intercalated with limestone conglo...

内陆棚以深、绿质泥岩夹浅砂质、质纹层条带为特征,并编制了该区桑塔木组的岩相图。

In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.

该油岩呈深棕褐 ,发育 ,主要由富含有机质纹层和浅钙质纹层形成的毫米级沉积层偶组成。

The platform foreslope is composed of the dark grey and celadon calcareous mudstone,siltstone,sandstone intercalated with limestone conglo...

内陆棚以深灰、灰绿灰质泥夹浅灰砂质、灰质纹层或条带为特征,并编制了该地区桑塔木相古地理图。

In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.

该油呈深灰或棕 ,理发育 ,主要由富含有机质纹层和浅灰钙质纹层形成毫米级沉积层偶成。

The platform foreslope is composed of the dark grey and celadon calcareous mudstone,siltstone,sandstone intercalated with limestone conglo...

内陆棚以、绿色质泥岩夹浅色砂质、质纹层或条带为特征,并编制了地区桑塔木组的岩相古地。

In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.

油岩色或棕褐色 ,发育 ,主要由富含有机质纹层和浅色钙质纹层形成的毫米级沉积层偶组成。

The platform foreslope is composed of the dark grey and celadon calcareous mudstone,siltstone,sandstone intercalated with limestone conglo...

内陆棚以深灰、灰绿灰泥岩夹浅灰砂、灰或条带为特征,并编制了该地区桑塔木组的岩相古地理图。

In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.

该油岩呈深灰或棕褐 ,理发育 ,主要由富含有机和浅灰形成的毫米级沉积偶组成。

The platform foreslope is composed of the dark grey and celadon calcareous mudstone,siltstone,sandstone intercalated with limestone conglo...

内陆棚以深、绿质泥岩夹浅砂质、质纹层条带为特征,并编制了该区桑塔木组的岩相图。

In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.

该油岩呈深棕褐 ,发育 ,主要由富含有机质纹层和浅钙质纹层形成的毫米级沉积层偶组成。

The platform foreslope is composed of the dark grey and celadon calcareous mudstone,siltstone,sandstone intercalated with limestone conglo...

内陆棚以深、绿色泥岩夹浅色、或条带为特征,并编制了该地区桑塔木组的岩相古地理图。

In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.

该油岩呈深色或棕褐色 ,理发育 ,主要由富含有机和浅色钙成的毫米级沉积偶组成。