Burial diagenesis causes a progressive transformation of smectites, the end-products being dependent on PH and pore water chemistry.

埋藏成岩作用可使蒙脱石进一步转化，最终产物决定PH孔隙水的化学性质。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化可见成岩早，而钾长石的钠长石化只发生成岩晚。

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.

经历成岩作用之前，含有燧石质的胶结成分。成岩作用过程中，低温抵压改变了沉积物的成分，而后固结成岩。

Burial diagenesis causes a progressive transformation of smectites, the end-products being dependent on PH and pore water chemistry.

埋藏岩使蒙脱石进一步转化，最终产物决定PH值及孔隙水的化学性质。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化见岩早期，而钾长石的钠长石化只发生岩晚期。

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.

在它经历岩之前，它含有燧石质的分。岩过程中，低温抵压改变了沉积物的分，而后固岩。

Burial diagenesis causes a progressive transformation of smectites, the end-products being dependent on PH and pore water chemistry.

埋藏成岩作用可使蒙脱进一步转化，最终产物决定PH值及孔隙水化学性质。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜化可见成岩早期，而化只发生成岩晚期。

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.

在它经历成岩作用之前，它含有燧质胶结成分。成岩作用过程中，低温抵压改变了沉积物成分，而后固结成岩。

Burial diagenesis causes a progressive transformation of smectites, the end-products being dependent on PH and pore water chemistry.

埋藏成岩作用可使蒙脱进一步转化，最终产物决定PH值及孔隙水化学性质。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜钠化可见成岩早期，而钾钠化只发生成岩晚期。

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.

在它经历成岩作用之前，它含有燧质胶结成分。成岩作用过程中，低温抵压改变了沉积物成分，而后固结成岩。

Burial diagenesis causes a progressive transformation of smectites, the end-products being dependent on PH and pore water chemistry.

埋藏岩使蒙脱石进一步转化，最终产物决定PH值及孔隙水的化学性质。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化见岩早期，而钾长石的钠长石化只发生岩晚期。

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.

在它经历岩之前，它含有燧石质的分。岩过程中，低温抵压改变了沉积物的分，而后固岩。

Burial diagenesis causes a progressive transformation of smectites, the end-products being dependent on PH and pore water chemistry.

埋藏岩作用可使蒙脱石进一步转，最终产物决定PH值及孔隙学性质。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石钠长石可见岩早期，而钾长石钠长石只发岩晚期。

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，它含有燧石质胶结分。岩作用过程中，低温抵压改变了沉积物分，而后固结岩。

Burial diagenesis causes a progressive transformation of smectites, the end-products being dependent on PH and pore water chemistry.

成可使蒙脱石进一步转化，最终产物决定PH值及孔隙水的化学性质。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化可见成早期，而钾长石的钠长石化只发生成晚期。

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.

在它经历成之前，它含有燧石质的胶结成分。成过程中，低温抵压改变了沉积物的成分，而后固结成。

Burial diagenesis causes a progressive transformation of smectites, the end-products being dependent on PH and pore water chemistry.

埋藏作用可使蒙脱石进一步转化，最终产物决定PH值及的化学性质。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化可见早期，而钾长石的钠长石化只发生期。

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。

Burial diagenesis causes a progressive transformation of smectites, the end-products being dependent on PH and pore water chemistry.

埋藏用可使蒙脱石进一步转化，最决定PH值及孔隙水的化学性质。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化可见早期，而钾长石的钠长石化只发生晚期。

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.

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

Burial diagenesis causes a progressive transformation of smectites, the end-products being dependent on PH and pore water chemistry.

埋藏成可使蒙脱石进一步转化，物决定PH值及孔隙水的化学性质。

Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.

因此，斜长石的钠长石化可见成早期，而钾长石的钠长石化只发生成晚期。

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.

在它经历成之前，它含有燧石质的胶结成分。成过程中，低温抵压改变了沉积物的成分，而后固结成。