The eclogites at western segment of Altyn Tagh tectonic belt occur as lens or boundins within quratz-feldspathic gniesses characterized by amphibolite-facies parageneses. It mainly experienced the prograde amphibolite-facies stage (P=6.06-8.70kb, t=615-690℃), peak eclogite-facies stage (P＞15kb, T=700-850℃), granulitic facies stage (P=11-14kb, T=750℃) and ampbiolite-facies stage (P=6.3-9.5kb, T=619-738℃) during decompression.
阿尔金构造带西段的榴辉岩呈透镜状产于长英质片麻岩中，它主要经历了进变质的角闪岩相(P=6.04-8.70Kb，T=615-690℃)、峰期的榴辉岩相(P＞15Kb，T=700-850℃)及减压过程中的麻粒岩相(P=11-14Kb，T=750℃)及角闪岩相(P=6.3-9.5，T=619-738℃)的变质作用，构成一个顺时针的PT轨迹。
I The metallotectonicses of Xitieshan Pb-Zn deposit in Qinghai Province have been demonstrated to belong to extensional metallotectonic series in ductile domain, and the Pb-Zn ore veins are controlled by the marble tectonic lens in the folding layers of metamorphic core complexes formed in Caledonian. ii The metallotectonicses of Woxi Au-Sb-W deposit in western Hunan Province have been discovered to belong to extensional metallotectonic series in brittle-ductile domain, and the bedded Au-Sb-W ore-veins are controlled by a bedded brittle-ductile shear zone with lowangle and down-slip. iii The metallotectonicses of Shuangwang gold deposit in Shanxi Province have been suggested to belong to hydrofracturing metallotectonic series, and the formation of the goldbearing hydroffacturing breccia bodies are caused by hydrofracturing of the deep-seated fluids with gold-bearing and rich-alkali in the rich sodium rocks of Devonian formed in hot-water sedimentation. iv The metallotectonicses, which controll quartz-vein type and alteration-rock type in Linglong-Jiaojia gold field, have been recongnized to belong to left-lateral strike—mormal slip metallotectonic series and normal—left-lateral strike slip metallotectonic series respectively, and their en echelon type, dip and dip-angle, pitch and pitch-angle are confined by the condiction of dynamics under the different tectonic regime. v The metallotectonicses of Jiangyong Ag-Pb-Zn deposit in Hunan Province have been identified to belong to karstic metallotectonic series and magmatic metallotectonic series respectively. vi The metallotectonicses of Xinhua gold deposit in Hunan Province have been found to belong to strike-slip metallotectonic series and extensional metallotectonic series respectively.
论证了青海锡铁山铅锌矿床的成矿构造属韧性域伸展成矿构造系列，脉状铅锌矿体受控于加里东期变质核杂岩的褶叠层中的大理岩构造透镜体；阐述了湘西沃溪金锑钨矿床的成矿构造属脆—韧性域伸展成矿构造系列，层状金锑钨矿体受控于低角度下滑型顺层脆—韧性剪切带；提出陕西双王金矿的成矿构造属水压成矿构造系列，含金水压角砾岩体是深源富碱含金流体在泥盆系一套热水沉积的富钠质岩系中发生水力压裂作用形成的；认为玲珑—焦家金矿田控制石英脉型和蚀变岩型的成矿构造分属左旋走滑—正滑成矿构造系列和正滑—左旋走滑成矿构造系列，两类金矿体的雁列型式、倾向与倾角以及侧伏向与侧伏角皆受上述不同构造体制下的动力学条件制约；厘定湖南江永县银铅锌矿的成矿构造分属岩溶成矿构造系列与岩浆成矿构造系列；发现湖南新化县金矿的成矿构造分属走滑成矿构造系列与伸展成矿构造系列。
I The metallotectonicses of Xitieshan Pb-Zn deposit in Qinghai Province have been demonstrated to belong to extensional metallotectonic series in ductile domain, and the Pb-Zn ore veins are controlled by the marble tectonic lens in the folding layers of metamorphic core complexes formed in Caledonian. ii The metallotectonicses of Woxi Au-Sb-W deposit in western Hunan Province have been discovered to belong to extensional metallotectonic series in brittle-ductile domain, andthe bedded Au-Sb-W ore-veins are controlled by a bedded brittle-ductile shear zone with lowangle and down-slip. iii The metallotectonicses of Shuangwang gold deposit in Shanxi Province have been suggested to belong to hydrofracturing metallotectonic series, and the formation of the goldbearing hydrofracturing breccia bodies are caused by hydrofractunng of the deep-seated fluids with gold-bearing and rich-alkali in the rich sodium rocks of Devonian formed in hot-water sedimentation. iv The metallotectonicses, which controll quartz-vein type and alteration-rock type in Linglong-Jiaojia gold field, have been recongnized to belong to left-lateral strike梞orrnal slip metallotectonic series and normal? left-lateral strike slip metallotectonic series respectively, and their en echelon type, dip and dip-angle, pitch and pitch-angle are confined by the condiction of dynamics under the different tectonic regime. v The metallotectonicses of Jiangyong Ag-Pb-Zn deposit in Hunan Province have been identified to belong to karstic metallotectonic series and magmatic metallotectonic series respectively. vi The metallotectonicses of Xinhua gold deposit in Hunan Province have been found to belong to strike-slip metallotectonic series and extensional metallotectonic series respectively.
论证了青海锡铁山铅锌矿床的成矿构造属韧性域伸展成矿构造系列，脉状铅锌矿体受控于加里东期变质核杂岩的褶叠层中的大理岩构造透镜体；阐述了湘西沃溪金锑钨矿床的成矿构造属脆—韧性域伸展成矿构造系列，层状金锑钨矿体受控于低角度下滑型顺层脆—韧性剪切带；提出陕西双王金矿的成矿构造属水压成矿构造系列，含金水压角砾岩体是深源富碱含金流体在泥盆系一套热水沉积的富钠质岩系中发生水力压裂作用形成的；认为玲拢—焦家金矿田控制石英脉型和蚀变岩型的成矿构造分属左族走滑—正滑成矿构造系列和正滑—左旋走滑成矿构造系列，两类金矿体的雁列型式、倾向与倾角以及侧伏向与侧伏角皆受上述不同构造体制下的动力学条件制约；厘定湖南江永县银铅锌矿的成矿构造分属岩溶成矿构造系列与岩浆成矿构造系列；发现湖南新化县金矿的成矿构造分属走滑成矿构造系列与伸展成矿构造系列。