Lithology and Mineral Resources最新文献_第2页

Sorption-Desorption of Rare-Earth Metal Cations by Ferromanganese Crusts of the Govorov Guyot, Magellan Seamounts, Pacific Ocean 太平洋麦哲伦海山戈沃罗夫-古约特铁锰结壳对稀土金属阳离子的吸附-解吸作用

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2024-09-02 DOI: 10.1134/S0024490224700640

G. V. Novikov, O. Yu. Bogdanova, N. V. Lobus, A. O. Rumayntseva

{"title":"Sorption-Desorption of Rare-Earth Metal Cations by Ferromanganese Crusts of the Govorov Guyot, Magellan Seamounts, Pacific Ocean","authors":"G. V. Novikov, O. Yu. Bogdanova, N. V. Lobus, A. O. Rumayntseva","doi":"10.1134/S0024490224700640","DOIUrl":"10.1134/S0024490224700640","url":null,"abstract":"The article presents the results of experimental studies of the sorption and desorption of rare-earth metal (REM) cations by the Co-bearing ferromanganese crusts of the Govorov Guyot. It has been established that the REM cations are sorbed on the CFC ore minerals (Fe-vernadite, vernadite, Mn-feroxyhite, and goethite. The crusts are characterized by high exchange capacity (1.78–3.57 mg-equiv/g, which increases in the following series: (Dy < Gd < Lu < Sm < Nd < Y, La < Eu) ( ll ) Ce. The REM cation sorption proceeds by the irreversible ion-exchange equivalent mechanism. The exchange complex of ore minerals consists of Na+, K+, Ca2+, and Mg2+ cations, which contribute 97‒98% to their total capacity. The crusts are characterized by the group sorption of REM cations from multicomponent water solutions of metal salts. The selectivity of manganese and ferruginous minerals of crusts to REM cations is significantly higher than to the main cations of ocean water. Experimental data on the desorption of sorbed REM cations with the NaCl solution suggest their irreversible sorption by ore minerals and strengthening of the chemical bond of sorbed REM cations with the main structural elements of these minerals over time. An important property of ore minerals, primarily manganese minerals, is their chemical and structural stability in aqueous electrolyte solutions, suggesting the repeated use of FMC as sorbents of REM cations.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"59 5","pages":"553 - 568"},"PeriodicalIF":0.7,"publicationDate":"2024-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142217767","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Geological Setting and Formation of the Erosional Structure of Upper Miocene Deposits in Western Ciscaucasia 西高加索上新世矿床的地质背景和侵蚀结构的形成

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2024-09-02 DOI: 10.1134/S0024490224700676

I. S. Postnikova, I. S. Patina, G. M. Gorkin

引用次数: 0

Lithogeochemistry of Upper Precambrian Terrigenous Rocks of Belarus: Communication 2. Provenance, Paleogeodynamics, Paleogeography, and Paleoclimate 白俄罗斯上前寒武纪土著岩石的岩石地球化学：交流 2.产状、古地球动力学、古地理学和古气候

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2024-09-02 DOI: 10.1134/S002449022470069X

A. V. Maslov, O. Yu. Melnichuk, A. B. Kuznetsov, V. N. Podkovyrov

{"title":"Lithogeochemistry of Upper Precambrian Terrigenous Rocks of Belarus: Communication 2. Provenance, Paleogeodynamics, Paleogeography, and Paleoclimate","authors":"A. V. Maslov, O. Yu. Melnichuk, A. B. Kuznetsov, V. N. Podkovyrov","doi":"10.1134/S002449022470069X","DOIUrl":"10.1134/S002449022470069X","url":null,"abstract":"This paper completes the examination of results of the study of lithogeochemical characteristics of a pilot collection of the Riphean–Vendian sandstones, siltstones, and claystones (last one based on the interpretation of results) in Belarus. Data on the age of detrital zircon published in recent years suggest that Upper Precambrian rocks of this region were sourced from the Osnitsk–Mikashevichi and the Trans-Scandinavian igneous belts, the Volyn–Brest large igneous province, rapakivi granites, as well as various rock associations of Sarmatia, Danopolonian orogen and Svecofennides. Based on the lithogeochemical characteristics, the distribution of data points of the studied clastic rocks on discriminant diagrams provides insight into the possible provenance, paleogeodynamic, paleogeographic, and paleoclimatic settings and suggests several conclusions. The considered Riphean–Vendian stratons in Belarus are composed mainly of erosion products of within-plate granitoids, as well as various island-arc and syncollisional felsic igneous rocks. The share of erosion products of mafic rocks among them generally does not exceed 30%. It is significant mainly in the Volyn Group rocks (erosion products of the Volyn–Brest large igneous province), as well as in some samples of the Nizov, Selyavy, and Kotlin formations (fragments of mafic rocks from other provenances?). The source-to-sink transport was accomplished mainly by large rivers. Paleogeodynamic settings varied from quite active to quite passive. The paleoclimate in catchment areas was most likely arid/semiarid in the Riphean. In the Vendian, it was humid and varied from subtropical in the Early Vendian (except the Glusk Formation) to tropical in the Late Vendian. The obtained results also make it possible to show some peculiarities of the known methods and techniques of paleoclimate reconstruction.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"59 5","pages":"479 - 503"},"PeriodicalIF":0.7,"publicationDate":"2024-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142217763","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Paleozoic and Cenozoic Reef Formation. An Attempt at Comparative Analysis 古生代和新生代岩礁形成。比较分析尝试

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2024-09-02 DOI: 10.1134/S0024490224700688

V. G. Kuznetsov

引用次数: 0

Structural and Crystal-Chemical Features of Mg-Rich Minerals of the Glauconite–Illite Series from Upper Proterozoic Deposits in Eastern and Northern Siberia 东西伯利亚和北西伯利亚上新生代矿床中褐铁矿-沸石系列富镁矿物的结构和晶体化学特征

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2024-09-02 DOI: 10.1134/S0024490224700664

B. A. Sakharov, T. A. Ivanovskaya, V. A. Drits, A. T. Savichev

{"title":"Structural and Crystal-Chemical Features of Mg-Rich Minerals of the Glauconite–Illite Series from Upper Proterozoic Deposits in Eastern and Northern Siberia","authors":"B. A. Sakharov, T. A. Ivanovskaya, V. A. Drits, A. T. Savichev","doi":"10.1134/S0024490224700664","DOIUrl":"10.1134/S0024490224700664","url":null,"abstract":"At the current level of research, a generalization of previously studied and new lithological-mineralogical, structural, and crystal-chemical characteristics of globular layer silicates (GLS) of the Mg-rich glauconite–illite series from Upper Proterozoic sections of eastern and northern Siberia (Uchur–Maya region, Anabar uplift) has been carried out. The classification of glauconite–illite minerals was carried out in accordance with recommendations of the International Nomenclature Committees for Mica and Clay Minerals, as well as based on the available literature and our own data. The Al index, i.e., (KAl = VIAl/[VIFe3+ + VIAl]), in minerals of the glauconite–illite series varies from 0.40 to 0.85; the content of Mg and K cations varies, respectively, from 0.51 to 0.75 and from 0.63 to 0.80 f.u. Application of the X-ray modeling method for diffraction patterns of the oriented and unoriented specimens of Upper Proterozoic GLS made it possible to determine the following properties: the content of swelling layers (4–10%), their types (mica, smectite, chlorite), the nature of the alternation (short-range order factor, R = 0), unit cell parameters c sin β, c cos β/a, and average value of parameter b (9.018–9.074 Å). The conditions of glauconite formation in the Upper Proterozoic basins are considered, and their influence on the structural and crystal-chemical features of Mg presence in hydrocarbons is discussed.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"59 5","pages":"526 - 537"},"PeriodicalIF":0.7,"publicationDate":"2024-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142217766","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Features of the REE Geochemistry and Genesis of Rocks and Ores of the Nchwaning Manganese Deposit (Kalahari Manganese Field, South Africa) 恩奇瓦宁（Nchwaning）锰矿藏岩石和矿石的 REE 地球化学特征和成因（南非卡拉哈里锰矿区

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2024-09-02 DOI: 10.1134/S0024490224700639

V. N. Kuleshov, A. Yu. Bychkov, A. I. Brusnitsyn

引用次数: 0

Unusual Mineralization in Basaltic Andesites of the Submarine Esmeralda Volcano (Mariana Island Arc) 埃斯梅拉达海底火山（马里亚纳岛弧）玄武安山岩中的异常成矿作用

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2024-07-13 DOI: 10.1134/S0024490224700585

V. A. Rashidov, V. V. Petrova, V. V. Ananyev, N. V. Gorkova

{"title":"Unusual Mineralization in Basaltic Andesites of the Submarine Esmeralda Volcano (Mariana Island Arc)","authors":"V. A. Rashidov, V. V. Petrova, V. V. Ananyev, N. V. Gorkova","doi":"10.1134/S0024490224700585","DOIUrl":"10.1134/S0024490224700585","url":null,"abstract":"The results of studies of a basaltic andesite sample (complicated by the mineralized fracture and voids, as well as fracture and gas voids filled with secondary mineralization) dredged on the submarine Esmeralda Volcano are presented. A detailed comparative study of the mineral composition of the substance lining the fracture, the near-fracture space, and the basaltic andesite part unaffected by secondary alterations made it possible to discover the presence of a mineral assemblage, which is atypical for the unaltered volcanic rocks, in the submarine Esmeralda Volcano. In the intra-fracture space and adjacent basaltic andesite zones, wide variation ranges of the plagioclase composition are recorded; isomorphism in the Fe–Ca pyroxene series is studied; REE oxides, hydroxides, and fluorohydroxides are studied; and variability in the composition of minerals of the magnetite–hematite series is shown. Tectonic movements in the previously formed basaltic andesites likely promoted the emergence of permeable zones, through which new portions of the melt leaked. In a limited space, high fluid gas saturation, temperature, and pressure fostered the extraction of metal compounds from the melt and host rocks.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"59 4","pages":"417 - 440"},"PeriodicalIF":0.7,"publicationDate":"2024-07-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141614616","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Lithology, Source Areas, and Formation Settings of the Upper Triassic Deposits of Southwestern Primorye 滨海边疆区西南部上三叠统矿床的岩性、产地和地层设置

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2024-07-13 DOI: 10.1134/S0024490224700603

A. I. Malinovsky

{"title":"Lithology, Source Areas, and Formation Settings of the Upper Triassic Deposits of Southwestern Primorye","authors":"A. I. Malinovsky","doi":"10.1134/S0024490224700603","DOIUrl":"10.1134/S0024490224700603","url":null,"abstract":"The paper considers the composition of sandy rocks from the Upper Triassic deposits of the Mongugai Formation of southwestern Primorye and presents the results of its paleogeodynamic interpretation. It has been established that, according to their mineralogical and geochemical parameters, sandstones are petrogenic, correspond to graywackes and, only partially, to lithite arenites, are characterized by a significant degree of geochemical maturity of the clastic material, and their formation occurred due to the erosion of significantly weathered parent rocks of the source areas. Generalization and paleogeodynamic interpretation of the data obtained indicate that sedimentation in the southwestern Primorye in the Late Triassic occurred in basins related to the active continental margin settings probably complicated by strike-slip dislocations along transform faults. The dominant source of detrital material was continental land: cratons and crystalline basement inliers surrounding the rift zones or along transform faults. Felsic granite-metamorphic complexes were eroded with the participation of sedimentary rocks enriched with ancient components. A secondary source was a deeply dissected continental-margin igneous arc, which supplied an additional amount of sialic material, as well as a small amount of the basic–intermediate volcaniclastic rocks into the basin. The U–Pb geochronological studies of detrital zircons from sandy rocks of the formation made it possible to establish the age and the possible position of igneous complexes, destruction of which formed the sediments.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"59 4","pages":"390 - 408"},"PeriodicalIF":0.7,"publicationDate":"2024-07-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141609814","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Lithology and Sedimentation Conditions of the Latest Cretaceous in the Klementyev Mountain Section (Eastern Crimea) 克莱门特耶夫山地段（东克里米亚）最新白垩纪的岩性和沉积条件

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2024-07-13 DOI: 10.1134/S0024490224700573

D. M. Korshunov, P. A. Proshina, I. P. Ryabov, B. G. Pokrovsky, V. A. Musatov

引用次数: 0

Manifestations of the Early Oligocene Solenovian Crisis on the Northern Shelf of the Eastern Paratethys 东帕拉特提斯北大陆架早新世索伦诺维危机的表现形式

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2024-07-13 DOI: 10.1134/S0024490224700615

I. S. Patina, G. M. Gorkin, I. S. Postnikova

{"title":"Manifestations of the Early Oligocene Solenovian Crisis on the Northern Shelf of the Eastern Paratethys","authors":"I. S. Patina, G. M. Gorkin, I. S. Postnikova","doi":"10.1134/S0024490224700615","DOIUrl":"10.1134/S0024490224700615","url":null,"abstract":"The results of studies of the regional structure of Solenovian deposits of the Early Oligocene Rupelian Stage in the Cisсaucasian–Caspian region, which represented the northern slope of Eastern Paratethys in the Cenozoic, are presented. The geological structure and paleogeographic conditions in the basin during the Solenovian (second half of Early Oligocene) were refined based on a comprehensive interpretation of geological and geophysical materials. The spatial consequences of the sea level drop in Eastern Paratethys during the Oligocene regressions are traced. The periodic draining of shelf areas is reflected in the structure of erosional unconformities and buried river incisions. It has been established that the most significant was the late Solenovian regression with a relative sea level drop by more than 500 m. Consequently, a prominent unconformity surface, complicated by river incisions, was formed in the sedimentary sequence in the shelf part of the paleobasin (Maikop seismic sequence). Erosion ledges and landslide bodies formed on the slopes, and basin-infill complexes were accumulated in depressions.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"59 4","pages":"381 - 389"},"PeriodicalIF":0.7,"publicationDate":"2024-07-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141609819","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0