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

内陆棚、绿色质泥岩夹浅色砂质、质纹层或条带为特征,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.

该油岩呈色或棕褐色 ,理发育 ,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...

内陆棚以灰、灰绿色灰质泥夹浅灰色砂质、灰质纹层或条带为特征,并编制了地区桑塔木组的相古地理。

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.

灰色或棕褐色 ,理发育 ,主要由富含有机质纹层和浅灰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、灰绿色灰质泥岩夹浅灰色砂质、灰质纹层或条带为特征,并编制区桑塔木组的岩相古理图。

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.

油岩呈深灰色或棕褐色 ,理发育 ,主含有机质纹层和浅灰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...

内陆棚以深灰、灰绿灰质泥岩夹浅灰砂质、灰质纹层或条带为特征,并编制了该地区桑塔岩相古地图。

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 ,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...

内陆棚以深灰、灰绿色灰质泥岩夹浅灰色砂质、灰质纹层或条带为特征,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.

该油岩呈深灰色或棕褐色 ,理发育 ,主要由富含有机质纹层和浅灰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、灰绿色灰质泥岩夹浅灰色砂质、灰质纹层或条带为特征,并编制了该地区桑的岩相古地图。

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.

该油岩呈深灰色或棕褐色 ,育 ,主要由富含有机质纹层和浅灰色钙质纹层形成的毫米级沉积层偶成。

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

内陆棚以深、绿质泥岩夹浅质、质纹层或条带为特征,并编制了该地区桑塔木组岩相古地理图。

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.

该油岩呈深或棕褐 ,理发育 ,主要由富含有机质纹层和浅钙质纹层毫米级沉积层偶组。

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、绿色质泥岩夹浅色砂质、质纹层或条带为特征,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.

该油岩呈色或棕褐色 ,理发育 ,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。