The beginning of intraplate (diwa type) activization must be attributed to Early Proterozoic, When thick continental earthcrust and thermodynamic conditions close to the present had estahlished.Precambrian activizatio...The beginning of intraplate (diwa type) activization must be attributed to Early Proterozoic, When thick continental earthcrust and thermodynamic conditions close to the present had estahlished.Precambrian activization (protodiwa) induced hypogene structural recaworking, deepseated laults and troughs development, gabbro-granite and subalkaline magtnatizm, zone metamorphism, magmatogenic and hydrothermal ore production,whicll proceeded regularly, that allows their timing.Protodiwa metallogeny contrasts with the previous Precambrian due to relatively increased petrogenic and ore elements differentiation. Elements of various geochemical origins and noncharacteristic of Early Precambrian are found.ore deposition appears determined by gabbro-diorite-granite, gabbroumonzonite-syenite-granite, gabbro-anorthosite-rapakivi granite differentiated magmatic series. Elements mode is controlled both by fractional crystallization and the alliance with fluid phase.Throughout Late Proterozoic diwa geodynamics remained uniform, the most intensive on the fringe of Early Proterozoic folded belts. This allows us suggest the post-collisional subduction activating mantle and lower litosphere, and mantle diapirs formation the motive forces of protodiwa activization.展开更多
The review of orogeny in the paper illustrates the differences between tectonic and mor-phogenic definitions,of which most geologists so far accept the former. Orogeny stands for mobilestages in the evolution of the c...The review of orogeny in the paper illustrates the differences between tectonic and mor-phogenic definitions,of which most geologists so far accept the former. Orogeny stands for mobilestages in the evolution of the crust. The author defines the diwa-type Orogeny in the frame of diwatheory as an assemblage of all geological processes during post-platformal tectonomagmatism, andthen divides it by the form and dynamics of crustobody into hybrid three subtypes: divergent, con-vergent and hybrid types.展开更多
There is a close relationship between occurrence of nonmetallic minerals and tectonic evolution of geosyncline, platform and diwa (geodepression) on the western margin of the Dongting diwa. Some results that (1) diwa ...There is a close relationship between occurrence of nonmetallic minerals and tectonic evolution of geosyncline, platform and diwa (geodepression) on the western margin of the Dongting diwa. Some results that (1) diwa tectonics is berfeficial for formation and preservation of nonmetallic minerals and (2) volcano-sedimentary altered ore deposits, saline deposits and organo-sedimentary ore deposits can be often found in diwa basins are gained.展开更多
Professor Chen Guoda,a department member of Academia Sinica,a tu-tor of doctoral and post-doctoral students in the Central South Univer-sity of Technology,has been engaged in geological teaching and researchfor more t...Professor Chen Guoda,a department member of Academia Sinica,a tu-tor of doctoral and post-doctoral students in the Central South Univer-sity of Technology,has been engaged in geological teaching and researchfor more than 50 years.His most important contribution is to found theworldwide praised Diwa theory,which enjoys high prestige in the geo-logical community.展开更多
This studied gold ore belt is giant and very important in China. Its regional tectonics and evolutional process are complicated. There are a few of view points on its geotec-tonic attribute in the Mesozoic and Cenozoi...This studied gold ore belt is giant and very important in China. Its regional tectonics and evolutional process are complicated. There are a few of view points on its geotec-tonic attribute in the Mesozoic and Cenozoic eras and on the type of its some gold ore deposits, especially, on one hosted in the pre-diwa geological bodies. On the basis of the diwa theory, the author discussed the regionalization, and its evolutional process, and some features of diwa tectono-magmatism and diwa type of gold mineralization in this belt. The author proposed that(1)the main body zone is a part of the diwa regime in the Mesozoic and Cenozoic eras, and(2)the diwa tectono-magmatism had a series of features such as universalism and violence, newborn, reform and superimposition, joining, inheritance, multiperiodic activity, complica-tion and so on. The gold mineralization formed in the diwa regime are called diwa type of golddeposits.In this paper the diwa type of endogenetic gold mineralization products hosted in the pre-diwa geological bodies in this zone is discussed in detail.展开更多
This paper is divided into three parts, The first part introduces diwa theory and its extendedor branch schools. The second part describes the introduction, citation, review and developmentof diwa theory by Chinese an...This paper is divided into three parts, The first part introduces diwa theory and its extendedor branch schools. The second part describes the introduction, citation, review and developmentof diwa theory by Chinese and foreign geoscientists. The third part gives a brief account of diwastructures occurring in different parts of the world.展开更多
The orogenic process of the Central Orogenic Belt (COB) of China can basically be divided into two stages. The first stage was in the period of geosynclinal inversion or in the period of convergence of ancient 1andmas...The orogenic process of the Central Orogenic Belt (COB) of China can basically be divided into two stages. The first stage was in the period of geosynclinal inversion or in the period of convergence of ancient 1andmasses. The second stage wholly occurred in an intracontinental environment within the diwa regime. The modern mountain ranges are rnainly the products of the second stage. This paper elaborates them in the light of information from different parts of the orogenic belt.展开更多
There are three diwa regions in South Siberia and West Mongolia. One of them is arranged in West Transbaikalia and was formed from Devonian till Carboniferous periods. Numerous deposits of tungsten , tin, molybdenum, ...There are three diwa regions in South Siberia and West Mongolia. One of them is arranged in West Transbaikalia and was formed from Devonian till Carboniferous periods. Numerous deposits of tungsten , tin, molybdenum, REE, synnyrites, urtites are genetically linked with intrusive rocks. The next diwa region is arranged in North Mongolia and South Buryatia. This diwa region was formed in the Late Paleozoic time. The deposits of molybdenum, tungsten, boron, iron, copper, beryllium are genetically linked with magmatic rocks of this region. The third region was formed in Devonian in West Mongollia. The magmatic rocks of this region are represented by alkaline granitoids. Some deposits of REE and rare metals are linked with these rocks.展开更多
A dynamic mechanism, "lower lithospheric delamination and extension of the Cathaysian Diwa-type orogens" , has been put forward to explain the formation of the Cenozoic continental-margin-spreading-belt in S...A dynamic mechanism, "lower lithospheric delamination and extension of the Cathaysian Diwa-type orogens" , has been put forward to explain the formation of the Cenozoic continental-margin-spreading-belt in Southeast China. The processes of formation and develop-ment for the belt are from the stage of the Cathaysian Diwa-type orogens at which compression and thickening of curstobodies prevailed, to the stage of the basin-and-range-type structures at which the late orogenic crustal extension occurred, and then to the stage of the epicontinental Diwa-type rifts at which the lithospheric extension took place.展开更多
This paper presents a quantitative analysis of Jurassic-Quaternary basement subsidence in the Delingha basin, a tensile basin and compressive mountain type diwa basin, and corrected for local sediment loading. Subside...This paper presents a quantitative analysis of Jurassic-Quaternary basement subsidence in the Delingha basin, a tensile basin and compressive mountain type diwa basin, and corrected for local sediment loading. Subsidence patterns have been investigated for the effects of erosion induced uplift by means of analytical estimation. The history of the Delingha basin has been divided into four stages: 204(?)~130 Ma (SⅠ ), 130~95 Ma (SⅡ ), 67~35 Ma (SⅢ ) and 35~0 Ma (SⅣ ), recording episodic tectonics and sedimentation respectively.展开更多
文摘The beginning of intraplate (diwa type) activization must be attributed to Early Proterozoic, When thick continental earthcrust and thermodynamic conditions close to the present had estahlished.Precambrian activization (protodiwa) induced hypogene structural recaworking, deepseated laults and troughs development, gabbro-granite and subalkaline magtnatizm, zone metamorphism, magmatogenic and hydrothermal ore production,whicll proceeded regularly, that allows their timing.Protodiwa metallogeny contrasts with the previous Precambrian due to relatively increased petrogenic and ore elements differentiation. Elements of various geochemical origins and noncharacteristic of Early Precambrian are found.ore deposition appears determined by gabbro-diorite-granite, gabbroumonzonite-syenite-granite, gabbro-anorthosite-rapakivi granite differentiated magmatic series. Elements mode is controlled both by fractional crystallization and the alliance with fluid phase.Throughout Late Proterozoic diwa geodynamics remained uniform, the most intensive on the fringe of Early Proterozoic folded belts. This allows us suggest the post-collisional subduction activating mantle and lower litosphere, and mantle diapirs formation the motive forces of protodiwa activization.
文摘The review of orogeny in the paper illustrates the differences between tectonic and mor-phogenic definitions,of which most geologists so far accept the former. Orogeny stands for mobilestages in the evolution of the crust. The author defines the diwa-type Orogeny in the frame of diwatheory as an assemblage of all geological processes during post-platformal tectonomagmatism, andthen divides it by the form and dynamics of crustobody into hybrid three subtypes: divergent, con-vergent and hybrid types.
文摘There is a close relationship between occurrence of nonmetallic minerals and tectonic evolution of geosyncline, platform and diwa (geodepression) on the western margin of the Dongting diwa. Some results that (1) diwa tectonics is berfeficial for formation and preservation of nonmetallic minerals and (2) volcano-sedimentary altered ore deposits, saline deposits and organo-sedimentary ore deposits can be often found in diwa basins are gained.
文摘Professor Chen Guoda,a department member of Academia Sinica,a tu-tor of doctoral and post-doctoral students in the Central South Univer-sity of Technology,has been engaged in geological teaching and researchfor more than 50 years.His most important contribution is to found theworldwide praised Diwa theory,which enjoys high prestige in the geo-logical community.
文摘This studied gold ore belt is giant and very important in China. Its regional tectonics and evolutional process are complicated. There are a few of view points on its geotec-tonic attribute in the Mesozoic and Cenozoic eras and on the type of its some gold ore deposits, especially, on one hosted in the pre-diwa geological bodies. On the basis of the diwa theory, the author discussed the regionalization, and its evolutional process, and some features of diwa tectono-magmatism and diwa type of gold mineralization in this belt. The author proposed that(1)the main body zone is a part of the diwa regime in the Mesozoic and Cenozoic eras, and(2)the diwa tectono-magmatism had a series of features such as universalism and violence, newborn, reform and superimposition, joining, inheritance, multiperiodic activity, complica-tion and so on. The gold mineralization formed in the diwa regime are called diwa type of golddeposits.In this paper the diwa type of endogenetic gold mineralization products hosted in the pre-diwa geological bodies in this zone is discussed in detail.
文摘This paper is divided into three parts, The first part introduces diwa theory and its extendedor branch schools. The second part describes the introduction, citation, review and developmentof diwa theory by Chinese and foreign geoscientists. The third part gives a brief account of diwastructures occurring in different parts of the world.
文摘The orogenic process of the Central Orogenic Belt (COB) of China can basically be divided into two stages. The first stage was in the period of geosynclinal inversion or in the period of convergence of ancient 1andmasses. The second stage wholly occurred in an intracontinental environment within the diwa regime. The modern mountain ranges are rnainly the products of the second stage. This paper elaborates them in the light of information from different parts of the orogenic belt.
文摘There are three diwa regions in South Siberia and West Mongolia. One of them is arranged in West Transbaikalia and was formed from Devonian till Carboniferous periods. Numerous deposits of tungsten , tin, molybdenum, REE, synnyrites, urtites are genetically linked with intrusive rocks. The next diwa region is arranged in North Mongolia and South Buryatia. This diwa region was formed in the Late Paleozoic time. The deposits of molybdenum, tungsten, boron, iron, copper, beryllium are genetically linked with magmatic rocks of this region. The third region was formed in Devonian in West Mongollia. The magmatic rocks of this region are represented by alkaline granitoids. Some deposits of REE and rare metals are linked with these rocks.
文摘A dynamic mechanism, "lower lithospheric delamination and extension of the Cathaysian Diwa-type orogens" , has been put forward to explain the formation of the Cenozoic continental-margin-spreading-belt in Southeast China. The processes of formation and develop-ment for the belt are from the stage of the Cathaysian Diwa-type orogens at which compression and thickening of curstobodies prevailed, to the stage of the basin-and-range-type structures at which the late orogenic crustal extension occurred, and then to the stage of the epicontinental Diwa-type rifts at which the lithospheric extension took place.
文摘This paper presents a quantitative analysis of Jurassic-Quaternary basement subsidence in the Delingha basin, a tensile basin and compressive mountain type diwa basin, and corrected for local sediment loading. Subsidence patterns have been investigated for the effects of erosion induced uplift by means of analytical estimation. The history of the Delingha basin has been divided into four stages: 204(?)~130 Ma (SⅠ ), 130~95 Ma (SⅡ ), 67~35 Ma (SⅢ ) and 35~0 Ma (SⅣ ), recording episodic tectonics and sedimentation respectively.
