New World Map of Large and Superlarge Mineral Deposits

Rundqvist, D. V.; Cherkasov, Sergei; Kutuzova, N.I.; Stavsky, A.P.

doi:10.1127/gtm/7/1999/131

Cited by 3 publications

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“…Most of the magmatic plutonogenic , volcanogenic and hydrothermal ore-mintral formation apparently have a mantle source of ore matter [13,19,27,48,50,100,115,130,153]. The bulk of stratiform type ore deposits occurring in sedimentary and metamorphic rocks are syngenetic and mixed origin, and the source of ore matter from deep-mantle and due to mobilization crustal rocks and ore-bearing formations [66,123]. A significant group of diverse deposits of sedimentary and metamorphic origin has a syngenetic source of ore formation [29,44,101,119,129,130] .…”

Section: Research Resultsmentioning

confidence: 99%

“…Sedimentary formations contain various mineral paragenesis [83,101] and complex relationships with each other [139]. Many sedimentary formations are ore-bearing and contain syngenetic ore deposits [19,20,24,66,115,123], contain significant reserves of minerals: hard and brown coal, oil and gas, bauxites, placers of various minerals and metals, gold, phosphorite, fresh and mineral waters. In the formation of sediments, rhythmicity, cyclicity and periodicity are noted [30,43,96,133] in accordance with the general regime of the gravity, magmatic activity, the dynamics of the Earth and sedimentation.…”

Section: Research Resultsmentioning

confidence: 99%

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The Dynamic Structural-Material Complexes of the Earth’s Crust

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2024

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Аннотация . Периодически развиваются самоподобные движения структурно-вещественных комплексов (СМК) из состава Солнечной системы в течение периода около 4,5 миллиардов лет земной коры, развития Земли в условиях самоорганизации. Синхронные или близкие во времени ряды генетических или парагенетических групп магматических, рудно-минеральных, метасоматических, осадочных образований, их структур и других сопутствующих им процессов, включают в себя каждый комплекс (ГМК). Каждый комплекс в его пределах ограничен во времени и пространстве, по причине признаков самопроизвольного динамического процесса; распространяется на территорию Земли в текущий исторический период; формирует состав и структуру земной коры на этом этапе, определяя ее полициклическое развитие. Количество циклов около 14,

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Section: Research Resultsmentioning

confidence: 99%

Section: Research Resultsmentioning

confidence: 99%

The Dynamic Structural-Material Complexes of the Earth’s Crust

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2024

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“…Most of the magmatic (plutonogenic), volcanogenic, and hydrothermal ore-mineral formations apparently have a mantle source of matter [48,50,153,130,19,27,100,115,13]. The bulk of stratiform type ore deposits occurring in sedimentary and metamorphic rocks are syngenetic and mixed origin, and the source of the ore matter from the deep mantle and due to the mobilization of crustal rocks and ore-bearing formations [ 66,123]. A significant group of diverse deposits of sedimentary and metamorphic origin has a syngenetic source of ore-mineral formation [129,130,29,101,44,119 ].…”

Section: The Complex Of Ore-mineral Formations Of the Earth's Crustmentioning

confidence: 99%

“…The sedimentary formations more often according to the material composition differences minerals paragenesis contains [101,83] and complex relationships with each other [139]. Many sedimentary formations are ore-bearing and syngenetic ore deposits contain [19,24,20,66,115,123], significant reserves of minerals: hard and brown coal, oil and gas, bauxites, placers of various minerals and metals, gold , phosphorite, fresh and mineral waters contains. For sediments rhythmicity, cyclicity, and periodicity are noted [96,133,30,43].…”

Section: The Complex Of the Sedimentary Formations Of The Earth's Crustmentioning

confidence: 99%

The Dynamic Structural-Material Complexes of the Earth’s Crust

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2023

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Annotation. The self-similar dynamic structural-material complexes (SMC) from the composition of the Solar System over a period of about 4.5 billion years of the earth's crust, of the Earth's development under the conditions of self-organization, are periodically formed. The synchronous or close-in-time series of genetically or paragenetically related igneous, ore-mineral, metasomatic, sedimentary formations, their structures, and other processes accompanying them, each complex (SMC) includes. Each complex in its formation is limited in time and space, according to the manifestation of the features of a spontaneous dynamic process; spreads in the volume of the Earth in a certain historical period; forms the composition and structure of the Earth's crust at this stage, its polycyclic development determining. The number of cycles is about 14, with decreasing duration of their manifestation.

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New Recognized Intellect for Prospecting Large‐superlarge Mineral Deposits

Rongfu

Mei

et al. 2012

Acta Geologica Sinica (Eng)

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Based on the data base of 1285 mineral deposits of 22 commodities in 121 countries of 6 continents of the world, the authors use the linear trend analysis for their reserves to determine the cut‐off limited order of reserves to select 36 exceptional superlarge (as peak mineral), 95 superlarge and 314 large deposits as new recognized intellect for their quantitative change. We have projected above 445 large‐superlarge deposits on (1:5 M) global tectonic background map and divided 4 metallogenic domains, 21 metallogenic belts. Global metallogeny of large‐superlarge deposits are: unity by endogenic, exogenic metamorphic and epigenetic in origin; speciality in different metallogenic domains and belts; preferentiality to ore‐forming elements of Cu, Au, Fe, Ag, Cr, Mn, Zn, Pb, Sb, Hg, to continental margins or plate convergent belts, to Intra‐continental tectono‐magmatic complex belts and Large ductile shear zones; abnormality by the global oxyatmversion (excess oxygen atmospheric event) in Archean, redoxyatmversion (lack oxygen atmospheric event) in Proterozoic‐Paleozoic, and tectonosphere thermal erosion (great amount of tectonic magmatic event) in Mesozoic‐Cenozoic.

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New World Map of Large and Superlarge Mineral Deposits

Cited by 3 publications

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The Dynamic Structural-Material Complexes of the Earth’s Crust

The Dynamic Structural-Material Complexes of the Earth’s Crust

The Dynamic Structural-Material Complexes of the Earth’s Crust

New Recognized Intellect for Prospecting Large‐superlarge Mineral Deposits

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