Palaeocurrent measurements suggest a northward direction,indicating that the Kunlun area was at low elevation.

中新世的沉积以细颗粒泥和砂为，表明物源区较远 ，古流域坡度较，距离较长。

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相古地理图。

Kapeng syderolite deposit is large,occurred in purple clayey ferruginous mudstone and grey-green clayey shale of Lower Silurian series.

卡棚大型紫砂陶土矿赋存于志留系下统紫红色粘土质含铁泥和灰绿色粘土质页中,分上下2个含矿系,4个矿层。

Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.

组成江汉盆地潜江凹陷潜江组盐间段非砂储层的为泥晶白云、钙芒硝、泥及其混积,孔渗性普遍较差。

And the boundary of them has the same lithologic character: the ravinement surface of river course or exposure mudstone of flooding plain and root clay.

二者的界面是相同的,均为河道砂体底部的冲刷侵蚀面或者是暴露过泛滥平原泥、根土等。

In the case of mudstone to be a source rock, the uncompacted mudstone would have a strong capability of hydrocarbon concentation sealing to seal gas in diffusive phase.

本文在研究盖层封闭油气机理的基础上,分析了欠压实泥在封益油气中的作用。

Palaeocurrent measurements suggest a northward direction,indicating that the Kunlun area was at low elevation.

中新世的沉积以泥岩和砂岩为主，表明物源区较远 ，古流域坡度较小，搬运距离较长。

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。

Kapeng syderolite deposit is large,occurred in purple clayey ferruginous mudstone and grey-green clayey shale of Lower Silurian series.

卡棚大型紫砂陶土矿主赋存于志留系下统紫红色粘土质含铁泥岩和灰绿色粘土质页岩中,分上下2个含矿岩系,4个矿层。

Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.

组成江汉盆地潜江凹陷潜江组盐间段非砂岩储层的岩石主为泥晶白云岩、钙芒硝岩、泥岩及其混积岩,孔渗较差。

And the boundary of them has the same lithologic character: the ravinement surface of river course or exposure mudstone of flooding plain and root clay.

二者的界面是相同的,均为河道砂体底部的冲刷侵蚀面或者是暴露过泛滥平原泥岩、根土岩等。

In the case of mudstone to be a source rock, the uncompacted mudstone would have a strong capability of hydrocarbon concentation sealing to seal gas in diffusive phase.

本文在研究盖层封闭油气机理的基础上,分析了欠压实泥岩在封益油气中的作用。

Palaeocurrent measurements suggest a northward direction,indicating that the Kunlun area was at low elevation.

中新世的沉积以细颗粒泥岩和砂岩为主，表明物源区较远 ，古流域坡度较小，搬运距离较长。

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。

Kapeng syderolite deposit is large,occurred in purple clayey ferruginous mudstone and grey-green clayey shale of Lower Silurian series.

卡棚大型紫砂陶土矿主赋存于志留系下统紫红色粘土质含铁泥岩和绿色粘土质页岩中,分上下2个含矿岩系,4个矿层。

Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.

组成汉地潜凹陷潜组盐间段非砂岩储层的岩石主为泥晶白云岩、钙芒硝岩、泥岩及其混积岩,孔渗性普遍较差。

And the boundary of them has the same lithologic character: the ravinement surface of river course or exposure mudstone of flooding plain and root clay.

二者的界面是相同的,均为河道砂体底部的冲刷侵蚀面或者是暴露过泛滥平原泥岩、根土岩等。

In the case of mudstone to be a source rock, the uncompacted mudstone would have a strong capability of hydrocarbon concentation sealing to seal gas in diffusive phase.

本文在研究盖层封闭油气机理的基础上,分析了欠压实泥岩在封益油气中的作用。

Palaeocurrent measurements suggest a northward direction,indicating that the Kunlun area was at low elevation.

中新世的沉积以细颗粒泥岩和岩为主，表明物源区较远 ，古流域坡度较小，搬运距离较长。

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。

Kapeng syderolite deposit is large,occurred in purple clayey ferruginous mudstone and grey-green clayey shale of Lower Silurian series.

卡棚大陶土矿主赋存于志统红色粘土质含铁泥岩和灰绿色粘土质页岩中,分上2个含矿岩,4个矿层。

Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.

组成江汉盆地潜江凹陷潜江组盐间段非岩储层的岩石主为泥晶白云岩、钙芒硝岩、泥岩及其混积岩,孔渗性普遍较差。

And the boundary of them has the same lithologic character: the ravinement surface of river course or exposure mudstone of flooding plain and root clay.

二者的界面是相同的,均为河道体底部的冲刷侵蚀面或者是暴露过泛滥平原泥岩、根土岩等。

In the case of mudstone to be a source rock, the uncompacted mudstone would have a strong capability of hydrocarbon concentation sealing to seal gas in diffusive phase.

本文在研究盖层封闭油气机理的基础上,分析了欠压实泥岩在封益油气中的作用。

Palaeocurrent measurements suggest a northward direction,indicating that the Kunlun area was at low elevation.

新世的沉积以细颗粒泥岩和砂岩为主，表明物源区较远 ，古流域坡度较小，搬运距离较长。

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古地理图。

Kapeng syderolite deposit is large,occurred in purple clayey ferruginous mudstone and grey-green clayey shale of Lower Silurian series.

卡棚大型紫砂陶土矿主赋存于志留系下统紫红色粘土质含铁泥岩和灰绿色粘土质页岩,分上下2个含矿岩系,4个矿层。

Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.

组成江汉盆地潜江凹陷潜江组盐间段非砂岩储层的岩石主为泥晶白云岩、钙芒硝岩、泥岩及其混积岩,孔渗性普遍较差。

And the boundary of them has the same lithologic character: the ravinement surface of river course or exposure mudstone of flooding plain and root clay.

二者的界同的,均为河道砂体底部的冲刷侵蚀或者暴露过泛滥平原泥岩、根土岩等。

In the case of mudstone to be a source rock, the uncompacted mudstone would have a strong capability of hydrocarbon concentation sealing to seal gas in diffusive phase.

本文在研究盖层封闭油气机理的基础上,分析了欠压实泥岩在封益油气的作用。

Palaeocurrent measurements suggest a northward direction,indicating that the Kunlun area was at low elevation.

中新世的沉积以细颗粒泥岩和砂岩为主，表明物源区较远 ，古流域坡度较小，搬运距离较长。

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,并编制了该区桑塔木组的岩相古。

Kapeng syderolite deposit is large,occurred in purple clayey ferruginous mudstone and grey-green clayey shale of Lower Silurian series.

卡棚大型紫砂陶矿主赋存于志留系下统紫红质含铁泥岩和灰绿质页岩中,分上下2个含矿岩系,4个矿层。

Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.

组成江汉盆潜江凹陷潜江组盐间段非砂岩储层的岩石主为泥晶白云岩、钙芒硝岩、泥岩及其混积岩,孔渗性普遍较差。

And the boundary of them has the same lithologic character: the ravinement surface of river course or exposure mudstone of flooding plain and root clay.

二者的界面是相同的,均为河道砂体底部的冲刷侵蚀面或者是暴露过泛滥平原泥岩、根岩等。

In the case of mudstone to be a source rock, the uncompacted mudstone would have a strong capability of hydrocarbon concentation sealing to seal gas in diffusive phase.

本文在研究盖层封闭油气机的基础上,分析了欠压实泥岩在封益油气中的作用。

Palaeocurrent measurements suggest a northward direction,indicating that the Kunlun area was at low elevation.

中新世的沉积以细颗粒泥和砂为主，表明物源区较远 ，流域坡度较小，搬运距离较长。

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、灰绿色灰泥夹浅灰色砂、灰纹层或条带为特征,并编制了该地区桑塔木组的地理图。

Kapeng syderolite deposit is large,occurred in purple clayey ferruginous mudstone and grey-green clayey shale of Lower Silurian series.

卡棚大型紫砂陶土矿主赋存于志留系下统紫红色粘土泥和灰绿色粘土页中,分上下2个矿系,4个矿层。

Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.

组成江汉盆地潜江凹陷潜江组盐间段非砂储层的石主为泥晶白云、钙芒硝、泥及其混积,孔渗性普遍较差。

And the boundary of them has the same lithologic character: the ravinement surface of river course or exposure mudstone of flooding plain and root clay.

二者的界面是同的,均为河道砂体底部的冲刷侵蚀面或者是暴露过泛滥平原泥、根土等。

In the case of mudstone to be a source rock, the uncompacted mudstone would have a strong capability of hydrocarbon concentation sealing to seal gas in diffusive phase.

本文在研究盖层封闭油气机理的基础上,分析了欠压实泥在封益油气中的作用。

Palaeocurrent measurements suggest a northward direction,indicating that the Kunlun area was at low elevation.

中新世的沉积以细颗粒泥岩和岩为主，表明物源区较远 ，古流域坡度较小，搬运距离较长。

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。

Kapeng syderolite deposit is large,occurred in purple clayey ferruginous mudstone and grey-green clayey shale of Lower Silurian series.

卡棚大陶土矿主赋存于志统红色粘土质含铁泥岩和灰绿色粘土质页岩中,分上2个含矿岩,4个矿层。

Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.

组成江汉盆地潜江凹陷潜江组盐间段非岩储层的岩石主为泥晶白云岩、钙芒硝岩、泥岩及其混积岩,孔渗性普遍较差。

And the boundary of them has the same lithologic character: the ravinement surface of river course or exposure mudstone of flooding plain and root clay.

二者的界面是相同的,均为河道体底部的冲刷侵蚀面或者是暴露过泛滥平原泥岩、根土岩等。

In the case of mudstone to be a source rock, the uncompacted mudstone would have a strong capability of hydrocarbon concentation sealing to seal gas in diffusive phase.

本文在研究盖层封闭油气机理的基础上,分析了欠压实泥岩在封益油气中的作用。

Palaeocurrent measurements suggest a northward direction,indicating that the Kunlun area was at low elevation.

中新世的沉积以细岩和砂岩为主，表明物源区较远 ，古流域坡度较小，搬运距离较长。

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。

Kapeng syderolite deposit is large,occurred in purple clayey ferruginous mudstone and grey-green clayey shale of Lower Silurian series.

卡棚大型紫砂陶土矿主赋存于志留系下统紫红色粘土质含铁岩和灰绿色粘土质页岩中,分上下2个含矿岩系,4个矿层。

Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.

组成江汉盆地潜江凹陷潜江组盐间段非砂岩储层的岩石主为晶白云岩、钙芒硝岩、岩及其混积岩,孔遍较差。

And the boundary of them has the same lithologic character: the ravinement surface of river course or exposure mudstone of flooding plain and root clay.

二者的界面是相同的,均为河道砂体底部的冲刷侵蚀面或者是暴露过泛滥平原岩、根土岩等。

In the case of mudstone to be a source rock, the uncompacted mudstone would have a strong capability of hydrocarbon concentation sealing to seal gas in diffusive phase.

本文在研究盖层封闭油气机理的基础上,分析了欠压实岩在封益油气中的作用。