{"id":14133,"date":"2023-04-16T07:03:08","date_gmt":"2023-04-16T12:03:08","guid":{"rendered":"http:\/\/library.chelscience.ru\/?page_id=14133"},"modified":"2023-04-28T13:09:03","modified_gmt":"2023-04-28T18:09:03","slug":"%d0%bf%d0%be%d1%81%d0%bb%d0%b5%d0%b4%d0%bd%d0%b8%d0%b5-%d0%bf%d0%be%d1%81%d1%82%d1%83%d0%bf%d0%bb%d0%b5%d0%bd%d0%b8%d1%8f","status":"publish","type":"page","link":"https:\/\/library.chelscience.ru\/?page_id=14133","title":{"rendered":"\u041d\u043e\u0432\u044b\u0435 \u043f\u043e\u0441\u0442\u0443\u043f\u043b\u0435\u043d\u0438\u044f"},"content":{"rendered":"\t\t
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\u041d\u043e\u0432\u044b\u0435 \u043f\u043e\u0441\u0442\u0443\u043f\u043b\u0435\u043d\u0438\u044f<\/h2>\n
\n \n \n\n \n \n \n \n\n\n col<\/th> ID<\/th> \u0410\u0432\u0442\u043e\u0440\u044b<\/th> \u041d\u0430\u0437\u0432\u0430\u043d\u0438\u0435 \u043f\u0443\u0431\u043b\u0438\u043a\u0430\u0446\u0438\u0438<\/th> \u0422\u0438\u043f<\/th> \u0413\u043e\u0434<\/th> \u041a\u043b\u044e\u0447\u0435\u0432\u044b\u0435 \u0441\u043b\u043e\u0432\u0430<\/th> \u0410\u043d\u043d\u043e\u0442\u0430\u0446\u0438\u044f<\/th> \u0421\u0442\u0440\u0430\u043d\u0438\u0446\u0430_\u043e\u0442<\/th> \u0421\u0442\u0440\u0430\u043d\u0438\u0446\u0430_\u0434\u043e<\/th> \u0421\u0442\u0440\u0430\u043d\u0438\u0446<\/th> \u0418\u0437\u0434\u0430\u0442\u0435\u043b\u044c\u0441\u0442\u0432\u043e<\/th> \u0423\u0414\u041a<\/th> PDF<\/th> \u0421\u0431\u043e\u0440\u043d\u0438\u043a<\/th> \u0420\u0435\u0434\u0430\u043a\u0442\u043e\u0440<\/th> \u0416\u0443\u0440\u043d\u0430\u043b<\/th> \u0422\u043e\u043c<\/th> \u041d\u043e\u043c\u0435\u0440<\/th> \u0412\u044b\u043f\u0443\u0441\u043a<\/th> DOI<\/th> URL<\/th> HTML<\/th> \u0418\u043d\u0432. \u2116<\/th> \u0421\u0442\u0435\u043b\u043b\u0430\u0436 <\/th> \u041f\u043e\u043b\u043a\u0430 <\/th> <\/tr>\n<\/thead>\n \n\n \n \n\n\n
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<\/td>\n 40249<\/td>\n \u041b\u0435\u0431\u0435\u0434\u0435\u0432\u0430 \u0410.\u0412., \u0411\u0435\u0440\u0437\u043e\u043d \u0415.\u0418., \u0411\u0430\u0433\u0430\u0435\u0432\u0430 \u0410.\u0410.<\/td>\n \u0413\u0435\u043e\u043b\u043e\u0433\u0438\u0447\u0435\u0441\u043a\u0430\u044f \u0445\u0430\u0440\u0430\u043a\u0442\u0435\u0440\u0438\u0441\u0442\u0438\u043a\u0430 \u0438 \u043e\u0441\u043e\u0431\u0435\u043d\u043d\u043e\u0441\u0442\u0438 \u0444\u043e\u0440\u043c\u0438\u0440\u043e\u0432\u0430\u043d\u0438\u044f \u043f\u043e\u0440\u0444\u0438\u0440\u043e\u0432\u043e\u0439 \u0441\u0438\u0441\u0442\u0435\u043c\u044b \u0428\u0438\u0440\u043e\u043a\u0438\u043d\u0441\u043a\u043e\u0433\u043e \u043c\u0430\u0441\u0441\u0438\u0432\u0430 (\u043f\u043e\u043b\u0443\u043e\u0441\u0442\u0440\u043e\u0432 \u0422\u0430\u0439\u043c\u044b\u0440)<\/td>\n \u0422\u0435\u0437\u0438\u0441\u044b<\/td>\n 2026<\/td>\n \u0442\u0430\u0439\u043c\u044b\u0440, \u0448\u0438\u0440\u043e\u043a\u0438\u043d\u0441\u043a\u0438\u0439 \u043c\u0430\u0441\u0441\u0438\u0432, \u043f\u043e\u0440\u0444\u0438\u0440\u043e\u0432\u0430\u044f \u0441\u0438\u0441\u0442\u0435\u043c\u0430, \u0434\u043e\u0440\u043e\u0436\u043d\u0438\u043d\u0441\u043a\u0438\u0439<\/td>\n <\/td>\n 18<\/td>\n 20<\/td>\n <\/td>\n <\/td>\n <\/td>\n \u0413\u0435\u043e\u043b\u043e\u0433\u0438\u044f XXI \u0432\u0435\u043a\u0430 – \u043f\u0435\u0440\u0435\u0434\u043e\u0432\u044b\u0435 \u0442\u0435\u0445\u043d\u043e\u043b\u043e\u0433\u0438\u0438 \u0438 \u043d\u0430\u0443\u0447\u043d\u043e-\u043c\u0435\u0442\u043e\u0434\u0438\u0447\u0435\u0441\u043a\u043e\u0435 \u043e\u0431\u0435\u0441\u043f\u0435\u0447\u0435\u043d\u0438\u0435 \u0440\u0435\u0433\u0438\u043e\u043d\u0430\u043b\u044c\u043d\u043e\u0433\u043e \u0433\u0435\u043e\u043b\u043e\u0433\u0438\u0447\u0435\u0441\u043a\u043e\u0433\u043e \u0438\u0437\u0443\u0447\u0435\u043d\u0438\u044f \u043d\u0435\u0434\u0440 \u0420\u043e\u0441\u0441\u0438\u0439\u0441\u043a\u043e\u0439 \u0424\u0435\u0434\u0435\u0440\u0430\u0446\u0438\u0438<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/tr>\n
<\/td>\n 40269<\/td>\n Wu X., Yu Ch., Zhao Z., Xu J., Ma X., Qin Y., Chen D., Tang H., Xu J., Li B., Liu Zh., Liu X., Wang Y.<\/td>\n Geochemical Characteristics of the Shuibutou Sedimentary Manganese Deposit in Southern Hunan Province, South China<\/td>\n \u0421\u0442\u0430\u0442\u044c\u044f<\/td>\n 2026<\/td>\n \u0448\u0443\u0439\u0431\u0443\u0442\u0443, \u043c\u0430\u0440\u0433\u0430\u043d\u0435\u0446, \u0445\u0443\u043d\u0430\u043d\u044c, \u043a\u0438\u0442\u0430\u0439, \u0433\u0435\u043e\u0445\u0438\u043c\u0438\u044f, \u043f\u0435\u0440\u043c\u044c, \u043a\u0438\u043b\u0438\u043d\u0433, \u0433\u0443\u0444\u0435\u043d\u0433<\/td>\n Permian sedimentary manganese carbonate deposits in the Qiling Basin exhibit substantial resource potential, yet their depositional environments and precipitation pathways remain insufficiently constrained. This study integrates petrographic, mineralogical, whole-rock geochemical, and carbonate C\u2013O isotope data from the Shuibutou Mn deposit in southern Hunan. We compare this deposit with the coeval Dongxiangqiao deposit and other Permian marine sedimentary Mn deposits to constrain its depositional setting, Mn-carbonate precipitation mechanisms, and potential Mn sources. The Shuibutou ores contain 10.88\u201317.18 wt.% MnO and are characterized by spherulitic\u2013oolitic textures, abundant bioclasts, and framboidal pyrite. Mo\u2013U enrichment indicates anoxic bottom waters, whereas the near-marine \u03b413Ccarb values of ore carbonates (\u22120.24\u2030 to 1.28\u2030) are consistent with precipitation within a marine carbonate system and suggest direct precipitation of Mn(II) carbonates from dissolved Mn2+ under anoxic conditions. In this setting, dissolved Mn2+ accumulated below the chemocline. Partial dissolution of platform-derived calcite grains near the chemocline increased local dissolved inorganic carbon and alkalinity, driving Mn-carbonate supersaturation and the authigenic precipitation of manganoan calcite, ultimately forming manganese carbonate ores. The low Al\/(Al + Fe + Mn) ratios, high Fe\/Ti ratios, and Co\u2013Ni\u2013Zn and REY geochemical characteristics are consistent with a possible contribution from Mn-rich deep fluids to the dissolved Mn2+ inventory of the basin waters. Similarities in mineralogy, geochemistry, and depositional setting between Shuibutou and Dongxiangqiao point to a possible regional role for the direct precipitation of Mn(II) carbonates under anoxic conditions in the Middle Permian Qiling Basin. Relatively deep intraplatform basins may therefore represent favorable targets for manganese carbonate exploration and provide a reference for exploration targeting of Permian sedimentary Mn deposits within the Qiling Basin.<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n Minerals<\/td>\n 16<\/td>\n 8<\/td>\n <\/td>\n 10.3390\/min16080858<\/td>\n <\/td>\n HTML<\/button><\/a><\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/tr>\n
<\/td>\n 40270<\/td>\n Waizy H., Moles N., Smith M.<\/td>\n Genesis of the Giant Aynak Copper Deposit, Afghanistan: Constraints from Sulphide Geochemistry (ICP-MS) and Fluid Inclusions<\/td>\n \u0421\u0442\u0430\u0442\u044c\u044f<\/td>\n 2026<\/td>\n \u0430\u0439\u043d\u0430\u043a, \u0430\u0444\u0433\u0430\u043d\u0438\u0441\u0442\u0430\u043d, \u043c\u0435\u0434\u043d\u043e\u043f\u043e\u0440\u0444\u0438\u0440\u043e\u0432\u044b\u0439<\/td>\n Located 30 km south\u2013southeast of Kabul in Logar province, Aynak is the largest and best-known copper orebody in Afghanistan. The deposit is hosted by the Loy Khwar Formation, a Neoproterozoic\u2013Cambrian metasedimentary sequence of dolomite marble, carbonaceous quartz schist and quartz\u2013biotite\u2013dolomite schist. The primary ore minerals are chalcopyrite and bornite, with less abundant pyrite and minor cobaltite, chalcocite, pyrrhotite, sphalerite and molybdenite. Sulphides occur as bedded laminae and disseminations, in metamorphic segregations, and in syn- to post-metamorphic cross-cutting veins. Building on the mineralogical, lithogeochemical and sulphur isotope framework established by Waizy et al. (2020), ICP-MS analyses of sulphide-rich separates from Central and Western Aynak (n = 31) were undertaken to characterise trace-element distributions, evaluate possible metal sources, and further constrain the genetic model of the deposit. Co and As enrichment in chalcopyrite-dominant samples is consistent with cobaltite, whereas Co enrichment in the absence of arsenic suggests the possible presence of carrollite. Fluid inclusion analyses of secondary quartz-hosted inclusions indicate interaction between the Aynak deposits and saline aqueous fluids (32 to 47 equivalent wt% NaCl) at minimum P-T conditions of ~100\u2013200 MPa and 300 \u00b0C. It is uncertain whether these fluid parameters relate to primary copper transport and deposition, or to remobilisation during metamorphism. Nevertheless, comparison with analogous sediment-hosted copper deposits suggests that highly saline basinal brines played an important role in the formation and evolution of the deposit. Occurrences of scapolite provide additional evidence for a model of brine-related mineralisation. Together with previously published mineralogical, lithogeochemical and sulphur isotope evidence, these findings support a sedimentary\u2013diagenetic origin for the Aynak copper deposit that is broadly comparable with sediment-hosted stratiform copper systems of the Central African Copperbelt.<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n Minerals<\/td>\n 16<\/td>\n 8<\/td>\n <\/td>\n 10.3390\/min16080844<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/tr>\n
<\/td>\n 40271<\/td>\n Belogub E., Brusnitsyn A., Novoselov K., Filippova K., Sadykov S.<\/td>\n Oolitic Ironstones and Carbonate Mn Ores of the Marsyaty Deposit (Northern Urals, Russia): A Key Study of Mineralogy and Geochemistry<\/td>\n \u0421\u0442\u0430\u0442\u044c\u044f<\/td>\n 2026<\/td>\n \u043c\u0430\u0440\u0441\u044f\u0442\u0441\u043a\u043e\u0435, \u0441\u0435\u0432\u0435\u0440\u043d\u044b\u0439 \u0443\u0440\u0430\u043b, poi, \u043e\u043e\u043b\u0438\u0442\u043e\u0432\u044b\u0439 \u0436\u0435\u043b\u0435\u0437\u043d\u044f\u043a, \u0437\u0430\u043f\u0430\u0434\u043d\u043e-\u0441\u0438\u0431\u0438\u0440\u0441\u043a\u0438\u0439 \u0431\u0430\u0441\u0441\u0435\u0439\u043d, \u0440\u043e\u0434\u043e\u0445\u0440\u043e\u0437\u0438\u0442\u043e\u0432\u044b\u0435 \u0440\u0443\u0434\u044b<\/td>\n This article describes the mineralogical and geochemical features of the Marsyaty Mn\u2013Fe sedimentary deposit in the Northern Urals (Russia). Oolitic ironstones of the deposit are localized in the Cenomanian coastal sandstones. Manganese ores (carbonate and carbonate\u2013oxide types) lies within the Lower Paleocene siliciclastic sediments and are separated from the oolitic ironstone (iron oxide and iron carbonate types) by a polymictic gravelite bed. Authigenic Fe3+ oxyhydroxides (goethite and ferrihydrite), chamosite\/berthierine and late siderite predominate in the ironstones; kaolinite, apatite, perhamite, calcite and dolomite are minor constituents. Rhodochrosite and rancieite are the major minerals of the manganese ore; Mn-dominated phyllosilicates (parsettensite? and caryopilite?) are rare. Both ore types contain authigenic glauconite, montmorillonite, sulfides (sphalerite\/wurtzite, galena, and pyrite), gibbsite\/boehmite and REE phosphates. Both ore types contain detrital quartz, ilmenite, zircon, monazite, epidote, titanite, muscovite and feldspars. The \u03b413Ccarb value (VPDB) varies from \u221218.5 to \u221223.3 in both ironstone types and from \u221210.0 to \u221241.0 \u2030 in the manganese ore. The negative C isotopic composition and numerous organic remains indicate the involvement of microbial processes in the formation of both types of carbonate ores. The Fe and Mn ores belong to one transgression\u2013regression sedimentation cycle and formed consecutively during the evolution of the West Siberian basin. A unique feature of the Marsyaty deposit includes two ore formation stages within a limited area and over a relatively short geological period: the accumulation of (i) oolitic ironstones enriched in Mn first and then (ii) manganese ores only.<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n Minerals<\/td>\n 16<\/td>\n 8<\/td>\n <\/td>\n 10.3390\/min16070756<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/tr>\n
<\/td>\n 40381<\/td>\n \u041d\u043e\u0432\u043e\u0441\u0435\u043b\u043e\u0432 \u041a.\u0410., \u0415.\u0412. \u0411\u0435\u043b\u043e\u0433\u0443\u0431 \u0415.\u0412., \u0424\u0438\u043b\u0438\u043f\u043f\u043e\u0432\u0430 \u041a.\u0410., \u0420\u0430\u0441\u0441\u043e\u043c\u0430\u0445\u0438\u043d \u041c.\u0410., \u0421\u0430\u0434\u044b\u043a\u043e\u0432 \u0421.\u0410.<\/td>\n \u041c\u0430\u0433\u043d\u0435\u0442\u0438\u0442\u043e\u0432\u044b\u0435 \u043f\u0435\u0441\u0447\u0430\u043d\u0438\u043a\u0438 \u0410\u0433\u0430\u0440\u0446\u0438\u043d\u0441\u043a\u043e\u0433\u043e Fe-Ti \u043c\u0435\u0441\u0442\u043e\u0440\u043e\u0436\u0434\u0435\u043d\u0438\u044f (\u0410\u0440\u043c\u0435\u043d\u0438\u044f): \u043c\u0438\u043d\u0435\u0440\u0430\u043b\u043e\u0433\u043e-\u0433\u0435\u043e\u0445\u0438\u043c\u0438\u0447\u0435\u0441\u043a\u0438\u0435 \u043e\u0441\u043e\u0431\u0435\u043d\u043d\u043e\u0441\u0442\u0438<\/td>\n \u0421\u0442\u0430\u0442\u044c\u044f<\/td>\n 2026<\/td>\n \u0430\u0440\u043c\u0435\u043d\u0438\u044f, \u0430\u0433\u0430\u0440\u0446\u0438\u043d, \u043c\u0430\u043b\u044b\u0439 \u043a\u0430\u0432\u043a\u0430\u0437, \u0436\u0435\u043b\u0435\u0437\u0438\u0441\u0442\u044b\u0439 \u043f\u0435\u0441\u0447\u0430\u043d\u0438\u043a<\/td>\n <\/td>\n 45<\/td>\n 65<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n \u041c\u0438\u043d\u0435\u0440\u0430\u043b\u043e\u0433\u0438\u044f<\/td>\n 12<\/td>\n 3<\/td>\n <\/td>\n 10.35597\/2313-545X-2026-12-3-3 <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/tr>\n
<\/td>\n 40393<\/td>\n Tatar C., Kalender L., Kara H., Al\u00e7i\u00e7ek \u00d6N Ar B.<\/td>\n Mineralogical Characteristics, Fluid Inclusions, C\u2013O Isotope Geochemistry, and Rb\u2013Sr Isotope Systematics of Listvenites Related to the Eastern Taurus Ophiolites, Malatya, T\u00fcrkiye<\/td>\n \u0421\u0442\u0430\u0442\u044c\u044f<\/td>\n 2026<\/td>\n \u0442\u0443\u0440\u0446\u0438\u044f, rb-sr, \u0442\u0430\u0443\u0440\u0443\u0441, \u043e\u0444\u0438\u043e\u043b\u0438\u0442, \u043b\u0438\u0441\u0442\u0432\u0435\u043d\u0438\u0442<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n Minerals<\/td>\n 16<\/td>\n <\/td>\n <\/td>\n 10.3390\/min16101015<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/tr>\n
<\/td>\n 40438<\/td>\n Li S-Y., Wu R.-Y., Huang T., Chen Sh-Y.<\/td>\n Orogenic and Post-Orogenic Gold Deposits: Spatiotemporal Distribution, Tectonic Controls, and Genetic Models<\/td>\n \u0421\u0442\u0430\u0442\u044c\u044f<\/td>\n 2026<\/td>\n \u043e\u0440\u043e\u0433\u0435\u043d\u043d\u044b\u0439, \u0433\u0435\u043d\u0435\u0442\u0438\u0447\u0435\u0441\u043a\u0430\u044f \u043c\u043e\u0434\u0435\u043b\u044c<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n Minerals<\/td>\n 16<\/td>\n 10<\/td>\n <\/td>\n 10.3390\/min16101052<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/tr>\n
<\/td>\n 40494<\/td>\n \u041d\u043e\u0432\u043e\u0441\u0435\u043b\u043e\u0432 \u041a.\u0410., \u0415.\u0412. \u0411\u0435\u043b\u043e\u0433\u0443\u0431 \u0415.\u0412., \u0411\u0440\u0443\u0441\u043d\u0438\u0446\u044b\u043d \u0410.\u0418.<\/td>\n \u041e\u043e\u043b\u0438\u0442\u043e\u0432\u044b\u0435 \u0436\u0435\u043b\u0435\u0437\u043d\u044f\u043a\u0438 \u0417\u0430\u0443\u0440\u0430\u043b\u044c\u044f<\/td>\n \u0421\u0442\u0430\u0442\u044c\u044f<\/td>\n 2026<\/td>\n poi, \u043e\u043e\u043b\u0438\u0442\u043e\u0432\u044b\u0439 \u0436\u0435\u043b\u0435\u0437\u043d\u044f\u043a, \u0437\u0430\u0443\u0440\u0430\u043b\u044c\u0435, \u043c\u0430\u0440\u0441\u044f\u0442\u0441\u043a\u043e\u0435, \u043c\u0443\u0433\u0430\u0439\u0441\u043a\u043e\u0435, \u0441\u0438\u043d\u0430\u0440\u043e-\u0442\u0435\u0447\u0435\u043d\u0441\u043a\u043e\u0435, \u0430\u044f\u0442\u0441\u043a\u043e\u0435<\/td>\n <\/td>\n 110<\/td>\n 113<\/td>\n <\/td>\n \u0415\u043a\u0430\u0442\u0435\u0440\u0438\u043d\u0431\u0443\u0440\u0433: \u0423\u0440\u041e \u0420\u0410\u041d<\/td>\n <\/td>\n <\/td>\n \u041e\u0441\u0430\u0434\u043e\u0447\u043d\u044b\u0435 \u043a\u043e\u043c\u043f\u043b\u0435\u043a\u0441\u044b \u0423\u0440\u0430\u043b\u0430 \u0438 \u0441\u043e\u043f\u0440\u0435\u0434\u0435\u043b\u044c\u043d\u044b\u0445 \u0440\u0435\u0433\u0438\u043e\u043d\u043e\u0432 \u0438 \u0438\u0445 \u043c\u0438\u043d\u0435\u0440\u0430\u0433\u0435\u043d\u0438\u044f – 2026<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/tr>\n
<\/td>\n 40502<\/td>\n Rogov M., Panchenko I.<\/td>\n Palaeogeographic, palaeoclimatic, and stratigraphic control of glendonite occurrences in the Jurassic and Cretaceous of Western Siberia and adjacent areas of the Yenisei-Khatanga Strait<\/td>\n \u0421\u0442\u0430\u0442\u044c\u044f<\/td>\n 2026<\/td>\n \u0437\u0430\u043f\u0430\u0434\u043d\u0430\u044f \u0441\u0438\u0431\u0438\u0440\u044c, \u044e\u0440\u0430, \u043c\u0435\u043b, \u043f\u0430\u043b\u0435\u043e\u0433\u0435\u043e\u0433\u0440\u0430\u0444\u0438\u044f, \u043f\u0430\u043b\u0435\u043e\u043a\u043b\u0438\u043c\u0430\u0442, \u0433\u043b\u0435\u043d\u0434\u043e\u043d\u0438\u0442, \u0435\u043d\u0438\u0441\u0435\u0439-\u0445\u0430\u0442\u0430\u043d\u0433\u0441\u043a\u0430\u044f \u0432\u043f\u0430\u0434\u0438\u043d\u0430<\/td>\n \u043e\u0431\u0437\u043e\u0440 https:\/\/dzen.ru\/a\/at4LUowtABJAT4ZD<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n Journal of Palaeogeography<\/td>\n 15<\/td>\n 5<\/td>\n <\/td>\n 10.1016\/j.jop.2026.100420<\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/td>\n <\/tr>\n
<\/td>\n 40511<\/td>\n Yao J., Han Y., Zhang D., Liu Q., Chen L., Cui P., Zhao G.<\/td>\n Material cycling across Earth\u2019s spheres and triggers of Cambrian explosion: a tectonic perspective<\/td>\n \u0421\u0442\u0430\u0442\u044c\u044f<\/td>\n 2026<\/td>\n \u043a\u0435\u043c\u0431\u0440\u0438\u0439\u0441\u043a\u0438\u0439 \u0432\u0437\u0440\u044b\u0432<\/td>\n \u0420\u0430\u0441\u043a\u043e\u043b \u0441\u0443\u043f\u0435\u0440\u043a\u043e\u043d\u0442\u0438\u043d\u0435\u043d\u0442\u0430
\u0426\u0435\u043f\u043e\u0447\u043a\u0430 \u043d\u0430\u0447\u0438\u043d\u0430\u0435\u0442\u0441\u044f \u0441 \u0440\u0430\u0441\u043f\u0430\u0434\u0430 \u0441\u0443\u043f\u0435\u0440\u043a\u043e\u043d\u0442\u0438\u043d\u0435\u043d\u0442\u0430 \u0420\u043e\u0434\u043e\u043d\u0438\u044f \u043f\u0440\u0438\u043c\u0435\u0440\u043d\u043e 850 \u043c\u0438\u043b\u043b\u0438\u043e\u043d\u043e\u0432 \u043b\u0435\u0442 \u043d\u0430\u0437\u0430\u0434. \u0420\u0430\u0441\u043a\u043e\u043b \u0441\u043e\u043f\u0440\u043e\u0432\u043e\u0436\u0434\u0430\u043b\u0441\u044f \u043c\u043e\u0449\u043d\u044b\u043c\u0438 \u0438\u0437\u0432\u0435\u0440\u0436\u0435\u043d\u0438\u044f\u043c\u0438: \u043b\u0430\u0432\u0430 \u0437\u0430\u0441\u0442\u044b\u0432\u0430\u043b\u0430 \u0432 \u0431\u0430\u0437\u0430\u043b\u044c\u0442, \u0430 \u0432 \u0430\u0442\u043c\u043e\u0441\u0444\u0435\u0440\u0443 \u043f\u043e\u043f\u0430\u0434\u0430\u043b \u0443\u0433\u043b\u0435\u043a\u0438\u0441\u043b\u044b\u0439 \u0433\u0430\u0437. \u0411\u0430\u0437\u0430\u043b\u044c\u0442 \u0440\u0430\u0437\u0440\u0443\u0448\u0430\u0435\u0442\u0441\u044f \u043f\u043e\u0434 \u0434\u043e\u0436\u0434\u0435\u043c \u0431\u044b\u0441\u0442\u0440\u0435\u0435 \u0431\u043e\u043b\u044c\u0448\u0438\u043d\u0441\u0442\u0432\u0430 \u043f\u043e\u0440\u043e\u0434 \u0438 \u043f\u0440\u0438 \u044d\u0442\u043e\u043c \u0437\u0430\u0431\u0438\u0440\u0430\u0435\u0442 \u0443\u0433\u043b\u0435\u043a\u0438\u0441\u043b\u044b\u0439 \u0433\u0430\u0437 \u0438\u0437 \u0432\u043e\u0437\u0434\u0443\u0445\u0430. \u0422\u0435\u043f\u043b\u0430 \u0441\u0442\u0430\u043b\u043e \u043c\u0435\u043d\u044c\u0448\u0435, \u043f\u043b\u0430\u043d\u0435\u0442\u0430 \u043e\u0441\u0442\u044b\u043b\u0430, \u0438 \u0431\u043e\u043b\u044c\u0448\u0430\u044f \u0435\u0435 \u0447\u0430\u0441\u0442\u044c \u043f\u043e\u043a\u0440\u044b\u043b\u0430\u0441\u044c \u043b\u044c\u0434\u043e\u043c \u2014 \u043d\u0430\u0441\u0442\u0443\u043f\u0438\u043b \u043f\u0435\u0440\u0438\u043e\u0434 \u00ab\u0417\u0435\u043c\u043b\u044f-\u0441\u043d\u0435\u0436\u043e\u043a\u00bb. \u041b\u0435\u0434 \u0431\u043b\u043e\u043a\u0438\u0440\u043e\u0432\u0430\u043b \u0441\u0432\u0435\u0442, \u0444\u043e\u0442\u043e\u0441\u0438\u043d\u0442\u0435\u0437 \u043e\u0441\u0442\u0430\u043d\u043e\u0432\u0438\u043b\u0441\u044f, \u0438 \u043e\u043a\u0435\u0430\u043d \u043f\u043e\u0447\u0442\u0438 \u043b\u0438\u0448\u0438\u043b\u0441\u044f \u043a\u0438\u0441\u043b\u043e\u0440\u043e\u0434\u0430. \u041f\u043e \u043c\u043d\u0435\u043d\u0438\u044e \u0430\u0432\u0442\u043e\u0440\u043e\u0432, \u0432 \u0442\u0430\u043a\u0438\u0445 \u0443\u0441\u043b\u043e\u0432\u0438\u044f\u0445 \u043c\u043d\u043e\u0433\u043e\u043a\u043b\u0435\u0442\u043e\u0447\u043d\u044b\u0435 \u043e\u0440\u0433\u0430\u043d\u0438\u0437\u043c\u044b \u043f\u043e\u043b\u0443\u0447\u0438\u043b\u0438 \u043f\u0440\u0435\u0438\u043c\u0443\u0449\u0435\u0441\u0442\u0432\u043e \u043f\u0435\u0440\u0435\u0434 \u043e\u0434\u043d\u043e\u043a\u043b\u0435\u0442\u043e\u0447\u043d\u044b\u043c\u0438. \u0422\u0430\u043b\u0430\u044f \u0432\u043e\u0434\u0430 \u0443 \u043a\u0440\u0430\u0435\u0432 \u043b\u0435\u0434\u043d\u0438\u043a\u043e\u0432 \u043c\u043e\u0433\u043b\u0430 \u043e\u0431\u0440\u0430\u0437\u043e\u0432\u044b\u0432\u0430\u0442\u044c \u043a\u0430\u0440\u043c\u0430\u043d\u044b, \u0431\u043e\u0433\u0430\u0442\u044b\u0435 \u043a\u0438\u0441\u043b\u043e\u0440\u043e\u0434\u043e\u043c. \u041a\u043e\u0433\u0434\u0430 \u043b\u0435\u0434\u043d\u0438\u043a\u0438 \u0440\u0430\u0441\u0442\u0430\u044f\u043b\u0438, \u043d\u0430\u0447\u0430\u043b\u0441\u044f \u0441\u0438\u043b\u044c\u043d\u044b\u0439 \u043f\u0430\u0440\u043d\u0438\u043a\u043e\u0432\u044b\u0439 \u044d\u0444\u0444\u0435\u043a\u0442. \u042d\u0442\u043e \u043a\u043e\u043b\u0435\u0431\u0430\u043d\u0438\u0435, \u043f\u043e \u0442\u0435\u043e\u0440\u0438\u0438 \u0438\u0441\u0441\u043b\u0435\u0434\u043e\u0432\u0430\u0442\u0435\u043b\u0435\u0439, \u043e\u0442\u043a\u0440\u044b\u043b\u043e \u043f\u0443\u0442\u044c \u043f\u0435\u0440\u0432\u044b\u043c \u043a\u0440\u0443\u043f\u043d\u044b\u043c \u0438 \u0441\u043b\u043e\u0436\u043d\u044b\u043c \u0444\u043e\u0440\u043c\u0430\u043c \u0436\u0438\u0437\u043d\u0438 \u2014 \u043c\u044f\u0433\u043a\u043e\u0442\u0435\u043b\u044b\u043c \u043e\u0440\u0433\u0430\u043d\u0438\u0437\u043c\u0430\u043c \u044d\u0434\u0438\u0430\u043a\u0430\u0440\u0441\u043a\u043e\u0433\u043e \u043f\u0435\u0440\u0438\u043e\u0434\u0430.

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\u0421\u0442\u043e\u043b\u043a\u043d\u043e\u0432\u0435\u043d\u0438\u044f \u043a\u043e\u043d\u0442\u0438\u043d\u0435\u043d\u0442\u043e\u0432 \u043f\u0440\u0438\u0432\u0435\u043b\u0438 \u043a \u043e\u0431\u0440\u0430\u0437\u043e\u0432\u0430\u043d\u0438\u044e \u0441\u0443\u043f\u0435\u0440\u043a\u043e\u043d\u0442\u0438\u043d\u0435\u043d\u0442\u0430 \u0413\u043e\u043d\u0434\u0432\u0430\u043d\u0430. \u041f\u0440\u0438\u043c\u0435\u0440\u043d\u043e \u0441 670 \u0434\u043e 440 \u043c\u0438\u043b\u043b\u0438\u043e\u043d\u043e\u0432 \u043b\u0435\u0442 \u043d\u0430\u0437\u0430\u0434 \u043d\u0430 \u043c\u0435\u0441\u0442\u0435 \u044d\u0442\u0438\u0445 \u0441\u0442\u043e\u043b\u043a\u043d\u043e\u0432\u0435\u043d\u0438\u0439 \u0432\u044b\u0440\u043e\u0441\u043b\u0438 \u0433\u043e\u0440\u043d\u044b\u0435 \u043f\u043e\u044f\u0441\u0430. \u0421\u0430\u043c\u044b\u0439 \u0434\u043b\u0438\u043d\u043d\u044b\u0439 \u0438\u0437 \u043d\u0438\u0445, \u043f\u043e \u043e\u0446\u0435\u043d\u043a\u0430\u043c, \u0442\u044f\u043d\u0443\u043b\u0441\u044f \u043e\u043a\u043e\u043b\u043e 9000 \u043a\u0438\u043b\u043e\u043c\u0435\u0442\u0440\u043e\u0432. \u0411\u043e\u043b\u044c\u0448\u0430\u044f \u0447\u0430\u0441\u0442\u044c \u0445\u0440\u0435\u0431\u0442\u043e\u0432 \u0440\u0430\u0441\u043f\u043e\u043b\u0430\u0433\u0430\u043b\u0430\u0441\u044c \u0432 \u0442\u0435\u043f\u043b\u044b\u0445 \u0438 \u0432\u043b\u0430\u0436\u043d\u044b\u0445 \u0448\u0438\u0440\u043e\u0442\u0430\u0445, \u0433\u0434\u0435 \u043f\u043e\u0440\u043e\u0434\u044b \u0431\u044b\u0441\u0442\u0440\u043e \u0440\u0430\u0437\u0440\u0443\u0448\u0430\u044e\u0442\u0441\u044f. \u0414\u043e\u0436\u0434\u0438 \u0440\u0430\u0437\u043c\u044b\u0432\u0430\u043b\u0438 \u0433\u043e\u0440\u044b, \u0430 \u0440\u0435\u043a\u0438 \u043d\u0435\u0441\u043b\u0438 \u0432 \u043c\u043e\u0440\u0435 \u043e\u0431\u043b\u043e\u043c\u043a\u0438 \u0438 \u043f\u0438\u0442\u0430\u0442\u0435\u043b\u044c\u043d\u044b\u0435 \u0432\u0435\u0449\u0435\u0441\u0442\u0432\u0430, \u043d\u0430\u043f\u0440\u0438\u043c\u0435\u0440 \u0444\u043e\u0441\u0444\u043e\u0440. \u0412 \u043e\u043a\u0435\u0430\u043d\u0435 \u043e\u043d\u0438 \u043a\u043e\u0440\u043c\u0438\u043b\u0438 \u0432\u043e\u0434\u043e\u0440\u043e\u0441\u043b\u0438 \u0438 \u0431\u0430\u043a\u0442\u0435\u0440\u0438\u0438, \u043a\u043e\u0442\u043e\u0440\u044b\u0435 \u0432\u044b\u0434\u0435\u043b\u044f\u043b\u0438 \u0431\u043e\u043b\u044c\u0448\u0435 \u043a\u0438\u0441\u043b\u043e\u0440\u043e\u0434\u0430. \u041e\u0441\u0430\u0434\u043a\u0438 \u043a \u0442\u043e\u043c\u0443 \u0436\u0435 \u043f\u043e\u0433\u0440\u0435\u0431\u0430\u043b\u0438 \u043c\u0435\u0440\u0442\u0432\u0443\u044e \u043e\u0440\u0433\u0430\u043d\u0438\u043a\u0443 \u0434\u043e \u0442\u043e\u0433\u043e, \u043a\u0430\u043a \u043e\u043d\u0430 \u0441\u0433\u043d\u0438\u0432\u0430\u043b\u0430 \u0438 \u0437\u0430\u0431\u0438\u0440\u0430\u043b\u0430 \u043a\u0438\u0441\u043b\u043e\u0440\u043e\u0434. \u0412 \u0438\u0442\u043e\u0433\u0435 \u043a\u0438\u0441\u043b\u043e\u0440\u043e\u0434 \u043d\u0430\u043a\u0430\u043f\u043b\u0438\u0432\u0430\u043b\u0441\u044f \u0432 \u0432\u043e\u0434\u0435 \u0438 \u0432 \u0432\u043e\u0437\u0434\u0443\u0445\u0435. \u0425\u0438\u043c\u0438\u0447\u0435\u0441\u043a\u0438\u0439 \u0441\u043e\u0441\u0442\u0430\u0432 \u0434\u0440\u0435\u0432\u043d\u0435\u0439 \u043c\u043e\u0440\u0441\u043a\u043e\u0439 \u0432\u043e\u0434\u044b \u043f\u043e\u0434\u0442\u0432\u0435\u0440\u0436\u0434\u0430\u0435\u0442 \u044d\u0442\u0443 \u043a\u0430\u0440\u0442\u0438\u043d\u0443: \u0441\u043e\u043e\u0442\u043d\u043e\u0448\u0435\u043d\u0438\u0435 \u0434\u0432\u0443\u0445 \u0444\u043e\u0440\u043c \u0441\u0442\u0440\u043e\u043d\u0446\u0438\u044f \u0442\u043e\u0433\u0434\u0430 \u0434\u043e\u0441\u0442\u0438\u0433\u043b\u043e \u043c\u0430\u043a\u0441\u0438\u043c\u0443\u043c\u0430 \u0437\u0430 \u0432\u0441\u044e \u0438\u0441\u0442\u043e\u0440\u0438\u044e \u0417\u0435\u043c\u043b\u0438.

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