The host rock conformably overlies a band of siliceous chertybrecia.

含矿主岩整合地上覆于硅角砾带之上。

This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

在它经历岩作用之前，它含有的胶结分。岩作用过程，抵压改变了沉积物的分，而后固结岩。

The host rock conformably overlies a band of siliceous chertybrecia.

含矿主岩整合地覆于硅角砾带之。

This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

在它经历岩作用之前，它含有的胶结分。岩作用过程中，低温抵压改变了沉积物的分，而后固结岩。

The host rock conformably overlies a band of siliceous chertybrecia.

含矿主地上覆于硅质燧石角砾石带之上。

This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

在它经历作用之前，它含有燧石质的胶结分。作用过程中，低温抵压改变了沉积物的分，而后固结。

The host rock conformably overlies a band of siliceous chertybrecia.

含矿主岩整合地上覆于硅质燧石角砾石带上。

This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

在它经历岩前，它含有燧石质的胶结分。岩过程中，低温抵压改变物的分，而后固结岩。

The host rock conformably overlies a band of siliceous chertybrecia.

含矿主岩整合地上覆于硅角砾带之上。

This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

在它经历岩作用之前，它含有的胶结分。岩作用过程，抵压改变了沉积物的分，而后固结岩。

The host rock conformably overlies a band of siliceous chertybrecia.

含矿主岩整合地上覆于硅质燧石角砾石带之上。

This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

历岩作用之前，含有燧石质的胶结。岩作用过程中，低温抵压改变了沉积物的，固结岩。

The host rock conformably overlies a band of siliceous chertybrecia.

含矿主整合地上覆于硅质燧带之上。

This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

在它经历作用之前，它含有燧质的胶结分。作用过程中，低温抵压改变了沉积物的分，而后固结。

The host rock conformably overlies a band of siliceous chertybrecia.

含矿主岩整合地上覆于硅质燧石角砾石带之上。

This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

在它经历岩作用之前，它含有燧石质的胶结。岩作用过程中，低温抵压改变了沉积物的，而后固结岩。

The host rock conformably overlies a band of siliceous chertybrecia.

含矿主岩整合地上覆于硅质燧石角砾石带上。

This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

在它经历岩作，它含有燧石质的胶结分。岩作过程中，低温抵压改积物的分，而后固结岩。