Eodiagenesis is characterized by the assemblage of carbonate-analcime-anhydrite, while authigenic kaolinite is found in some strata.

浅埋藏期以碳酸盐～沸石～硬石膏组合为特征。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

矿石由黄铁矿、闪锌矿、自然金、辉锑铅矿、砷黝铜矿、辉锑矿、辉锑银铅矿、雄黄、雌黄等组,为典型的低温热液矿物组合。

When the regional extension is disharmonic with the basement structure and movement, complicated fault assemblages can be form during progressive deformation.

上，结合理论分析，提出了复杂断层组合因的另一种模式——不协调伸展递进变形模式。

Eodiagenesis is characterized by the assemblage of carbonate-analcime-anhydrite, while authigenic kaolinite is found in some strata.

浅埋藏期以碳酸盐～沸石～硬石膏组合为特征。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

矿石由黄铁矿、闪锌矿、自然金、辉锑铅矿、砷黝铜矿、辉锑矿、辉锑银铅矿、雄黄、雌黄等组,为典型的低温热液矿物组合。

When the regional extension is disharmonic with the basement structure and movement, complicated fault assemblages can be form during progressive deformation.

在此，结合理论分析，提出了复杂断层组合因的另一种模式——不协调伸展递进变形模式。

Eodiagenesis is characterized by the assemblage of carbonate-analcime-anhydrite, while authigenic kaolinite is found in some strata.

浅埋藏期以碳酸盐～沸～硬合为特征。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

矿由黄铁矿、闪锌矿、自然金、辉锑铅矿、砷黝铜矿、辉锑矿、辉锑银铅矿、雄黄、雌黄等,为典型的低温热液矿物合。

When the regional extension is disharmonic with the basement structure and movement, complicated fault assemblages can be form during progressive deformation.

在此基础上，结合理论分析，提出了复杂断层合因的另一种模式——不协调伸展递进变形模式。

Eodiagenesis is characterized by the assemblage of carbonate-analcime-anhydrite, while authigenic kaolinite is found in some strata.

浅埋藏期以碳酸盐～沸石～硬石膏为特征。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

矿石由铁矿、闪锌矿、自然金、辉锑铅矿、砷黝铜矿、辉锑矿、辉锑银铅矿、、等,为典型的低温热液矿物。

When the regional extension is disharmonic with the basement structure and movement, complicated fault assemblages can be form during progressive deformation.

在此基础上，结理论分析，提出了复杂断层因的另一种模式——不协调伸展递进变形模式。

Eodiagenesis is characterized by the assemblage of carbonate-analcime-anhydrite, while authigenic kaolinite is found in some strata.

浅埋藏期以碳酸盐～沸石～硬石膏组合为特征。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

石由黄铁、闪锌、自然金、铅、砷黝铜、、银铅、雄黄、雌黄等组,为典型的低温热液物组合。

When the regional extension is disharmonic with the basement structure and movement, complicated fault assemblages can be form during progressive deformation.

在此基础上，结合理论分析，提出了复杂断层组合因的另一种模式——不协调伸展递进变形模式。

Eodiagenesis is characterized by the assemblage of carbonate-analcime-anhydrite, while authigenic kaolinite is found in some strata.

浅埋藏期以碳酸盐～沸石～硬石膏组合为特征。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

矿石矿、闪锌矿、自然金、辉锑铅矿、砷黝铜矿、辉锑矿、辉锑银铅矿、雄、雌等组,为典型的低温热液矿物组合。

When the regional extension is disharmonic with the basement structure and movement, complicated fault assemblages can be form during progressive deformation.

在此基础上，结合理论分析，提出了复杂断层组合因的另一种模式——不协调伸展递进变形模式。

Eodiagenesis is characterized by the assemblage of carbonate-analcime-anhydrite, while authigenic kaolinite is found in some strata.

浅埋藏期以碳酸盐～沸～硬膏组合为特征。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

黄铁、闪锌、自然金、辉锑铅、砷黝铜、辉锑、辉锑银铅、雄黄、雌黄等组,为典型的低温热液物组合。

When the regional extension is disharmonic with the basement structure and movement, complicated fault assemblages can be form during progressive deformation.

在此基础上，结合理论分析，提出了复杂断层组合因的另一种模式——不协调伸展递进变形模式。

Eodiagenesis is characterized by the assemblage of carbonate-analcime-anhydrite, while authigenic kaolinite is found in some strata.

浅埋藏期以碳酸盐～沸石～硬石膏组合为特征。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

矿石由黄铁矿、闪锌矿、自然金、辉锑铅矿、砷黝铜矿、辉锑矿、辉锑银铅矿、雄黄、雌黄等组,为典低温热液矿物组合。

When the regional extension is disharmonic with the basement structure and movement, complicated fault assemblages can be form during progressive deformation.

在此基础上，结合理论分析，提出了复杂断层组合因另一种模式——不协调伸展递进变形模式。

Eodiagenesis is characterized by the assemblage of carbonate-analcime-anhydrite, while authigenic kaolinite is found in some strata.

浅埋藏期以碳酸盐～沸石～硬石膏合为特征。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

石由黄铁、闪锌、自然金、辉锑铅、砷黝铜、辉锑、辉锑银铅、雄黄、雌黄等,为典型低温热液合。

When the regional extension is disharmonic with the basement structure and movement, complicated fault assemblages can be form during progressive deformation.

在此基础上，结合理论分析，提出了复杂断层合因另种模式——不协调伸展递进变形模式。