Nonconventional types of noble-, rare-metal, and rare-earth mineralization in coal-bearing basins in the far east

Sorokin, A. V.; Chanturia, V. A.; Rozhdestvina, V. I.; Kuz’minykh, V. M.; Жмодик, С. М.

doi:10.1134/s1028334x12100182

Cited by 18 publications

(12 citation statements)

References 3 publications

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“…The available data point to high contents of noble and other rare metals, including REE, in coal basins in the Russian Far East and China (Bakulin and Cherepanov, 2003;Cherepanov, 2008;Kuz'minykh and Sorokin, 2004;Rozhdestvina and Sorokin, 2010;Seredin, 2007;Sorokin et al, 2009Sorokin et al, , 2012Vyalov et al, 2010). (2)); 3, rocks of pre-Mesozoic basement; 4, boundary of coaliferous deposits; 5, brown-coal deposits and occurrences; 6, brown-coal sampling localities.…”

Section: Localization Of Coal-and Gold-bearing Structures Spatial Pamentioning

confidence: 96%

“…Since that time, NM mineralization has been revealed in many coal basins of Siberia, Transbaikalia, Far East, Ukraine, Bashkiria, Bulgaria, United Kingdom, Kazakhstan, Uzbekistan, Tajikistan, China, and other countries. Much attention has been focused on the use of other commercial components of coals, which requires, first of all, study of rare-metal mineralization, prospects for extraction of valuable and commercial components, development of the technology of complex processing of raw material, and solution of ecological problems of coaliferous deposits (Arbuzov et al, 2000;Cherepovskii, 1997;Ivanov, 2004;Ketris and Yudovich, 2009;Kizil'shtein et al, 1988;Krapiventseva, 2005;Leonov et al, 1998;Meitov, 2001;Mitkin et al, 2010;Ratynskii et al, 1982a,b;Rozhdestvina and Sorokin, 2010;Shpirt et al, 1999;Seredin and Finkelman, 2008;Sorokin et al, 2009Sorokin et al, , 2012Valiev et al, 1993;Rikhvanov et al, 1994;Yudovich et al, 1985;Yudovich and Ketris, 1986;Zhang et al, 2002).…”

Section: Introductionmentioning

confidence: 97%

“…Their genetic types, species present in coals, migration and transition forms during natural processes, and conditions of localization are investigated. Special attention is given to Russian Geology and Geophysics 54 (2013) [671][672][673][674][675][676][677][678][679][680][681][682][683][684] the physicochemical processes of their interaction with organic matter (Abramov et al, 1993;Buryak and Bakulin, 1998;Chukhrov, 1955;Chyi, 1982;Dai et al, 2003;Finkelman and Aruscavage, 1981;Fisher et al, 1974;Mitkin et al, 2010;Oman et al, 1997;Rozhdestvina and Sorokin, 2010;Seredin, 1997Seredin, , 2002Seredin, , 2004Seredin and Finkelman, 2008;Sorokin et al, 2009Sorokin et al, , 2012Varshal et al, 1984Varshal et al, , 1990Varshal et al, , 1994Varshal et al, , 2000Yudovskaya et al, 2003).…”

Section: Introductionmentioning

confidence: 99%

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The regularities of formation of noble- and rare-metal mineralization in Cenozoic coaliferous deposits in the southern Far East

Сорокин

Rozhdestvina

Kuz’minykh

et al. 2013

Russian Geology and Geophysics

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We performed system studies of age parageneses and lateral conjugation of peat and gold accumulation areas as well as the regularities of formation of noble-and rare-metal mineralization in Cenozoic coaliferous deposits in the south of the Russian Far East. The migration properties of noble metals (NMs) and their behavior in different media are considered. Based on literature data and results of experimental studies, we performed analysis and selection of the most optimal methods for the quantitative determination of NMs and trace and rare-earth elements. The experiments have confirmed the NB fugacity and have shown for the first time the scales of transportation of NMs as ultrafine particles during coal combustion. The obtained results significantly expand the notions of the migration properties of NMs and serve as the key to the solution of the problem of NM extraction in analytical and technological processes. Also, areas promising for noble-and rare-metal mineralization have been revealed in coal basins.

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Section: Localization Of Coal-and Gold-bearing Structures Spatial Pamentioning

confidence: 96%

Section: Introductionmentioning

confidence: 97%

Section: Introductionmentioning

confidence: 99%

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The regularities of formation of noble- and rare-metal mineralization in Cenozoic coaliferous deposits in the southern Far East

Сорокин

Rozhdestvina

Kuz’minykh

et al. 2013

Russian Geology and Geophysics

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“…They are related to the deltas of the river systems of the Ol'doi, Dep, Tom, and others of the same age draining the above men tioned uplifts. In the junction zone of the gold bearing provinces and coal fields, the Cenozoic peatbogs are enriched in noble, trace, and rare earth metals [22]. These events were related to the different mechanisms and transportation conditions: dissolved mobile spe cies of elements transferred with surface waters from the supergene zones of ore lodes, mineralized ground waters, species consumed and sorbed by coal forming plants and organic matter of caustobioliths of the coal series (as a geochemical barrier), clastogenic and ultrafine particles in association with clay minerals transported with water flows that drained source areas, air masses, etc.…”

Section: Brown Coalmentioning

confidence: 99%

Geological and geophysical interpretation of the detailed geophysical data on the Lower Zeya region of the Zeya-Bureya sedimentary basin

Сорокин

Kaplun

Malyshev

et al. 2015

Russ. J. of Pac. Geol.

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In 2010-2012, the Lower Zeya basin was studied by magnetotelluric sounding accompanied by gas geochemical sampling. The results of the geophysical studies provide sufficient insight into the large geo logical structures with a measurement step of 5 km and detail of individual elements (boundaries of troughs and rises and the cover thickness) with a step of 1 km. It was established that the MTS method highlights the block structure of the Lower Zeya basin, the inner structure of troughs, the style of the uplift-depression junction, and the regmatic framework of the region. Gas geochemical studies were used to decipher faults established from geophysical methods and to identify high permeability zones. The helium and hydrogen anomalies found in the soils suggest that these zones served as the fluid pathways. In some cases, our studies made it possible to outline the localization of many mineral resources.

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“…Согласно аналитическим данным А. П. Сорокина с соавт. [27], большинство ценных элементов-примесей в углях представлено рассеянными тонкими минеральными фазами. Например, в углях Ерковецкого буроугольного месторождения Амурской области обнаружены минералы различных классов.…”

Section: Introductionunclassified

Model experiments with multicomponent solutions and fungal biomass: the possibility of metalliferous biomineralization in coal accumulation

Павлова¹,

Radomskaya²,

Shumilova³

et al. 2019

Vestnik IG KomiSC

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1 Институт геологии и природопользования ДВО РАН, Благовещенск; pav@ascnet.ru 2 Дальневосточный геологический институт ДВО РАН, Владивосток В ñòàòьå пðåдñòàвëåíы ðåзóëьòàòы ìîдåëьíых экñпåðèìåíòîв пî èзвëå÷åíèю хèìè÷åñкèх эëåìåíòîв èз ìíîãîкîìпîíåíòíых ðàñòвîðîв бèîìàññîй ìèкðîñкîпè÷åñкèх ãðèбîв. Пîëó÷åííыå дàííыå ñвèдåòåëьñòвóюò î òîì, ÷òî ñîðбöèîííîå ñðîдñòвî эëåìåíòîв к ãðèбíîй бèîìàññå кàк ñîðбåíòó ñîîòвåòñòвóåò ñëåдóющåìó ðядó:As ≈ Ni ≈ Sr, кîòîðый îòðàжàåò íåпðîñòîй хàðàкòåð взàèìîдåйñòвèя è взàèìîвëèяíèя эëåìåíòîв в ìíîãîкîìпîíåíòíîй ñèñòåìå. С пîìîщью ñкàíèðóющåй эëåкòðîííîй ìèкðîñкîпèè íà ãðèбíîй бèîìàññå îбíàðóжåíы пîëèìåòàëëьíыå íîвîîбðàзîвàíèя ñëîжíîãî ñîñòàвà, пðåдñòàвëåííыå òîíкèìè кñåíîìîðфíыìè ÷àñòèöàìè (фàзàìè, зåðíàìè), à òàкжå хîðîшî îãðàíåííыìè кðèñòàëëàìè, èх ñðîñòкàìè è двîйíèкàìè, ÷òî дîкàзывàåò пîòåíöèàëьíóю вîзìîжíîñòь ìàñшòàбíîãî ìåòàëëîíîñíîãî бèîìèíåðàëîîбðàзîвàíèя в îðãàíîãåííых ñåдèìåíòîëèòàх. Сëîжíый ìåхàíèзì èзвëå-÷åíèя хèìè÷åñкèх эëåìåíòîв èз ìíîãîкîìпîíåíòíых ðàñòвîðîв ðåàëèзóåòñя в íåñкîëькî эòàпîв: пåðвîíà÷àëьíый эòàп íà-÷èíàåòñя ñ фèзèкî-хèìè÷åñкîй ñîðбöèè (зà ñ÷åò эëåкòðîñòàòè÷åñкîãî è вàí-дåð-вààëьñîвîãî взàèìîдåйñòвèй), в дàëьíåйшåì пðîòåкàåò èîííый îбìåí èëè кîìпëåкñîîбðàзîвàíèå ñ пîñëåдóющèì вîññòàíîвëåíèåì íåкîòîðых ñîðбèðîвàííых èîíîв ìåòàëëîв.Ключевые слова: элåìåíты, ìíîгîкîìпîíåíтíыå ðàствîðы, èçвлå÷åíèå, бèîсîðбöèя, ìèкðîскîпè÷åскèå гðèбы, бèîгåííîå ìèíåðàлîîбðàçîвàíèå, óглè.The results of model experiments on the extraction of chemical elements from multicomponent solutions by microscopic fungi biomass are presented in the article. The data obtained indicate that the chemical elements sorption affinity to the fungal biomass as a sorbent accords with following series: Bi ≈ Sn ≈ Pb ≈ Fe ≈ Hg ≈ (Sb) ≈ Cr> Cd ≈ Zn ≈ Cu ≈ V ≈ Se> Co ≈ Mn ≈ (Sb) ≈ As ≈ Ni ≈ Sr, which reflects the complex nature of the elements interaction and interinfluence in the multicomponent system. Polymetal neoplasms of complex composition, represented by thin xenomorphic particles (phases, grains), as well as well-faceted crystals, their intergrowths and twin son fungal biomass, were discovered by the method of analytical scanning electron microscopy, which proves the potentiality of extensive metal-bearing biomineralization in organogenic sedimentolites. The extraction complex mechanism of chemical elements from multicomponent solutions is implemented in stages: initial physicochemical sorption (due to electrostatic and Van der Waals interactions), further ion exchange or complexation, followed by some sorbed metal ions recovery.

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Nonconventional types of noble-, rare-metal, and rare-earth mineralization in coal-bearing basins in the far east

Cited by 18 publications

References 3 publications

The regularities of formation of noble- and rare-metal mineralization in Cenozoic coaliferous deposits in the southern Far East

The regularities of formation of noble- and rare-metal mineralization in Cenozoic coaliferous deposits in the southern Far East

Geological and geophysical interpretation of the detailed geophysical data on the Lower Zeya region of the Zeya-Bureya sedimentary basin

Model experiments with multicomponent solutions and fungal biomass: the possibility of metalliferous biomineralization in coal accumulation

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