Permian bioclastic limestone and bioherm are the most favorable reservoirs.

二叠系屑灰岩和为最有的储层。

According to the conodont and fusulinid fossils,their ages are determined to be Devonian-Permian.

所含化石确定地层形成时代为泥盆纪至二叠纪。

Along with the similarly large dinocephalia, the bradysaurs constituted the herbivorous megafauna of the late Middle Permian Period.

缓龙与类似大小的恐��兽类都是中二叠纪的草食性巨型土壤。

At the end of the Permian period the earth's landmasses were configured into one supercontinent, Pangea, and a superocean, Panthalassa.

二叠纪末期，地球上的陆地合并成一块超级大洲，叫作盘古大陆，以及一个超级大海，叫作原始大洋。

The secondary dolomite and paleokarst of the Lower Permian Series in Sichuan Basin is one of the important atectonic reserviors in the basin.

四川盆地下二叠统中次白云岩及古岩溶是下二叠统主要的非构造圈闭储层之一。

Permian bioclastic limestone and bioherm are the most favorable reservoirs.

二叠系生屑灰岩和生物礁最有的储层。

According to the conodont and fusulinid fossils,their ages are determined to be Devonian-Permian.

根据所含化石确定地层形成时盆纪至二叠纪。

Along with the similarly large dinocephalia, the bradysaurs constituted the herbivorous megafauna of the late Middle Permian Period.

缓龙与类似大小的恐��兽类都是中二叠纪的草食性巨型土壤生物。

At the end of the Permian period the earth's landmasses were configured into one supercontinent, Pangea, and a superocean, Panthalassa.

二叠纪末期，地球上的陆地合并成一块超级大洲，叫作盘古大陆，以及一个超级大海，叫作原始大洋。

The secondary dolomite and paleokarst of the Lower Permian Series in Sichuan Basin is one of the important atectonic reserviors in the basin.

四川盆地下二叠统中次生白云岩及古岩溶是下二叠统主要的非构造圈闭储层之一。

Permian bioclastic limestone and bioherm are the most favorable reservoirs.

二叠系生和生物礁为最有的储层。

According to the conodont and fusulinid fossils,their ages are determined to be Devonian-Permian.

根据所含定地层形成时代为泥盆纪至二叠纪。

Along with the similarly large dinocephalia, the bradysaurs constituted the herbivorous megafauna of the late Middle Permian Period.

缓龙与类似大小的恐��兽类都是中二叠纪的草食性巨型土壤生物。

At the end of the Permian period the earth's landmasses were configured into one supercontinent, Pangea, and a superocean, Panthalassa.

二叠纪末期，地球上的陆地合并成一块超级大洲，叫作盘古大陆，以及一个超级大海，叫作原始大洋。

The secondary dolomite and paleokarst of the Lower Permian Series in Sichuan Basin is one of the important atectonic reserviors in the basin.

四川盆地下二叠统中次生白云及古溶是下二叠统主要的非构造圈闭储层之一。

Permian bioclastic limestone and bioherm are the most favorable reservoirs.

二叠系生屑灰岩和生物礁为最有的储层。

According to the conodont and fusulinid fossils,their ages are determined to be Devonian-Permian.

根据所含化石确定地层形成时代为泥盆纪至二叠纪。

Along with the similarly large dinocephalia, the bradysaurs constituted the herbivorous megafauna of the late Middle Permian Period.

缓龙与类似小的恐��兽类都是中二叠纪的草食性巨型土壤生物。

At the end of the Permian period the earth's landmasses were configured into one supercontinent, Pangea, and a superocean, Panthalassa.

二叠纪末期，地球上的陆地合并成一块超洲，叫作盘古陆，以及一个超，叫作原始洋。

The secondary dolomite and paleokarst of the Lower Permian Series in Sichuan Basin is one of the important atectonic reserviors in the basin.

四川盆地下二叠统中次生白云岩及古岩溶是下二叠统主要的非构造圈闭储层之一。

Permian bioclastic limestone and bioherm are the most favorable reservoirs.

二叠系生屑灰岩和生物礁为最有的储层。

According to the conodont and fusulinid fossils,their ages are determined to be Devonian-Permian.

根据所含化石确定地层形成时代为泥盆纪至二叠纪。

Along with the similarly large dinocephalia, the bradysaurs constituted the herbivorous megafauna of the late Middle Permian Period.

缓龙与类似大小的恐��兽类都是中二叠纪的草食性巨型土壤生物。

At the end of the Permian period the earth's landmasses were configured into one supercontinent, Pangea, and a superocean, Panthalassa.

二叠纪末期，地球上的陆地合并成级大洲，叫作盘古大陆，以及个级大海，叫作原始大洋。

The secondary dolomite and paleokarst of the Lower Permian Series in Sichuan Basin is one of the important atectonic reserviors in the basin.

四川盆地下二叠统中次生白云岩及古岩溶是下二叠统主要的非构造圈闭储层之。

Permian bioclastic limestone and bioherm are the most favorable reservoirs.

二叠系生屑灰岩和生物礁最有的储层。

According to the conodont and fusulinid fossils,their ages are determined to be Devonian-Permian.

根据所含化石确定地层形成时代纪至二叠纪。

Along with the similarly large dinocephalia, the bradysaurs constituted the herbivorous megafauna of the late Middle Permian Period.

缓龙与类似大小的恐��兽类都是中二叠纪的草食性巨型土壤生物。

At the end of the Permian period the earth's landmasses were configured into one supercontinent, Pangea, and a superocean, Panthalassa.

二叠纪末期，地球上的陆地合并成一块超级大洲，叫作盘古大陆，以及一个超级大海，叫作原始大洋。

The secondary dolomite and paleokarst of the Lower Permian Series in Sichuan Basin is one of the important atectonic reserviors in the basin.

四川地下二叠统中次生白云岩及古岩溶是下二叠统主要的非构造圈闭储层之一。

Permian bioclastic limestone and bioherm are the most favorable reservoirs.

系生屑灰岩和生物礁为最有储层。

According to the conodont and fusulinid fossils,their ages are determined to be Devonian-Permian.

根据所含化石确定地层形成时代为泥盆至。

Along with the similarly large dinocephalia, the bradysaurs constituted the herbivorous megafauna of the late Middle Permian Period.

缓龙与类似大小恐��兽类都是中草食性巨型土壤生物。

At the end of the Permian period the earth's landmasses were configured into one supercontinent, Pangea, and a superocean, Panthalassa.

末期，地球上陆地合并成一块超级大洲，叫作盘古大陆，以及一个超级大海，叫作原始大洋。

The secondary dolomite and paleokarst of the Lower Permian Series in Sichuan Basin is one of the important atectonic reserviors in the basin.

四川盆地下统中次生白云岩及古岩溶是下统主要非构造圈闭储层之一。

Permian bioclastic limestone and bioherm are the most favorable reservoirs.

二系生屑灰岩和生物礁为最有储层。

According to the conodont and fusulinid fossils,their ages are determined to be Devonian-Permian.

根据所含化石确定层形成时代为泥盆至二。

Along with the similarly large dinocephalia, the bradysaurs constituted the herbivorous megafauna of the late Middle Permian Period.

缓龙与类似大小恐��兽类都是中二草食性巨型土壤生物。

At the end of the Permian period the earth's landmasses were configured into one supercontinent, Pangea, and a superocean, Panthalassa.

二末期，球上陆合并成一块超级大洲，叫作盘古大陆，以及一个超级大海，叫作原始大洋。

The secondary dolomite and paleokarst of the Lower Permian Series in Sichuan Basin is one of the important atectonic reserviors in the basin.

四川盆下二统中次生白云岩及古岩溶是下二统主要非构造圈闭储层之一。

Permian bioclastic limestone and bioherm are the most favorable reservoirs.

二叠系生屑灰岩和生物礁为有层。

According to the conodont and fusulinid fossils,their ages are determined to be Devonian-Permian.

根据所含化石确定地层形成时代为泥盆纪至二叠纪。

Along with the similarly large dinocephalia, the bradysaurs constituted the herbivorous megafauna of the late Middle Permian Period.

缓龙与类似大小恐��兽类都是中二叠纪草食性巨型土壤生物。

At the end of the Permian period the earth's landmasses were configured into one supercontinent, Pangea, and a superocean, Panthalassa.

二叠纪末期，地球上陆地合并成一块超级大洲，叫作盘古大陆，以及一个超级大海，叫作原始大洋。

The secondary dolomite and paleokarst of the Lower Permian Series in Sichuan Basin is one of the important atectonic reserviors in the basin.

四川盆地下二叠统中次生白云岩及古岩溶是下二叠统主要非构造圈闭层之一。

Permian bioclastic limestone and bioherm are the most favorable reservoirs.

二叠系生和生物礁为最有的储层。

According to the conodont and fusulinid fossils,their ages are determined to be Devonian-Permian.

根据所含定地层形成时代为泥盆纪至二叠纪。

Along with the similarly large dinocephalia, the bradysaurs constituted the herbivorous megafauna of the late Middle Permian Period.

缓龙与类似大小的恐��兽类都是中二叠纪的草食性巨型土壤生物。

At the end of the Permian period the earth's landmasses were configured into one supercontinent, Pangea, and a superocean, Panthalassa.

二叠纪末期，地球上的陆地合并成一块超级大洲，叫作盘古大陆，以及一个超级大海，叫作原始大洋。

The secondary dolomite and paleokarst of the Lower Permian Series in Sichuan Basin is one of the important atectonic reserviors in the basin.

四川盆地下二叠统中次生白云及古溶是下二叠统主要的非构造圈闭储层之一。