Lithology and Mineral Resources最新文献

Rare Metal—Titanium Placer Deposits in the East European and West Siberian Megaprovinces of Russia: Genesis, Geological Characteristics, Mineralogy, and Significance in the Titanium and Zirconium Mineral Resource Base 东欧和俄罗斯西伯利亚西部大省稀有金属-钛砂矿床：成因、地质特征、矿物学及其在钛锆矿产资源基地的意义

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2026-09-02 DOI: 10.1134/S0024490226600298

A. V. Lalomov, R. Seltmann, A. Dolgopolova, E. N. Levchenko, A. B. Makeyev, A. A. Bochneva

引用次数: 0

U–Th–Pb (LA-ICP-MS) Isotopic Age of Detrital Zircon from Sandstones of the Burzyan Group (Yamantau Anticlinorium, Southern Urals) 南乌拉尔亚曼托背斜布尔兹彦群砂岩碎屑锆石U-Th-Pb （LA-ICP-MS）同位素年龄

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2026-09-02 DOI: 10.1134/S0024490226600250

A. V. Maslov, V. B. Ershova, S. A. Dub, L. V. Badida, M. T. Krupenin, O. Yu. Melnichuk

{"title":"U–Th–Pb (LA-ICP-MS) Isotopic Age of Detrital Zircon from Sandstones of the Burzyan Group (Yamantau Anticlinorium, Southern Urals)","authors":"A. V. Maslov, V. B. Ershova, S. A. Dub, L. V. Badida, M. T. Krupenin, O. Yu. Melnichuk","doi":"10.1134/S0024490226600250","DOIUrl":"10.1134/S0024490226600250","url":null,"abstract":"The U–Th–Pb isotope age of detrital zircon populations from sandstones of the Bol’shoi Inzer and Yusha formations of the Burzyan Group (Lower Riphean) of the Yamantau Anticlinorium in the Southern Urals was analyzed. The presence of grains supplied to the sedimentation area from proximal and distal sources was demonstrated. The former likely included the Taratash Complex/Orogen and the Bak 1 complex of the Bakaly granitoid block of the Volga–Ural region, or rock associations similar in age and composition from other regions. The latter include the Volga–Don, Svecofennian, East Sarmatian, and other Early Proterozoic orogens of the East European Craton (Baltica). Considering the intracratonic nature of the Early Riphean sedimentation basin, it has been suggested that some of the detrital material could be delivered from non-Baltica/Siberian sources. Maximum sedimentation age of the Bol’shoi Inzer and Yusha formations has been established. The age of the Bol’shoi Inzer Formation is estimated at 1805 ± 30 Ma (according to the YSG algorithm) and 1870 Ma (according to the YPP algorithm). The Yusha Formation is characterized by the maximum sedimentation age of 1798 ± 10 and 1890 Ma, respectively.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"61 5","pages":"515 - 541"},"PeriodicalIF":0.7,"publicationDate":"2026-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148871816","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

Kaolinite‒Smectite from Deposits on Holocene Terraces of the Black Sea Coast of the Caucasus (Northwest of the Colchis Lowland) 高加索黑海沿岸全新世阶地沉积物中的高岭石-蒙脱石（Colchis低地西北部）

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2026-09-02 DOI: 10.1134/S0024490226600274

B. A. Sakharov, T. A. Sadchikova, G. V. Trebeleva

{"title":"Kaolinite‒Smectite from Deposits on Holocene Terraces of the Black Sea Coast of the Caucasus (Northwest of the Colchis Lowland)","authors":"B. A. Sakharov, T. A. Sadchikova, G. V. Trebeleva","doi":"10.1134/S0024490226600274","DOIUrl":"10.1134/S0024490226600274","url":null,"abstract":"Holocene terrace systems and isolated terraces have been identified on the Black Sea coast of the Caucasus, including the northwestern part of the Colchis Lowland. Their composition was studied using a combination of lithological and physicochemical methods. It has been shown that the fine fraction (<0.001 mm) of sediments consists predominantly of newly formed mixed-layer kaolinite‒smectite with a terrigenous admixtures of smectite, kaolinite, micaceous mineral, and occasionally chlorite. Using diffraction pattern modeling for air-dry and ethylene glycol-saturated natural samples, the structural parameters of clay minerals and their quantitative content were determined. No correlation was found between these parameters and the facies settings in which the terrace deposits formed. No correlation was also found between the structural parameters of kaolinite‒smectite and the depth of sediment occurrence or their location within the study area. All samples contain kaolinite‒smectite with a fairly narrow range of the ratio of kaolinite and smectite layers, Wk : Wsm, on average from 0.55 : 0.45 to 0.65 : 0.35. It is shown that the average crystallochemical formula calculated for kaolinite‒smectite with Wk : Wsm = 0.65 : 0.35 exactly corresponds to the dioctahedral structure of the mineral. The decomposition of this formula into smectite and kaolinite components indicates that the 1 : 1 layers in the studied kaolinite‒smectites differ in their crystallochemical structure from true kaolinite ones. A solid-phase mechanism for the formation of kaolinite‒smectites in a smectite matrix is proposed via the removal of fragments of tetrahedral sheets from 2 : 1 layers and adjacent smectite interlayers. The structural evolution of mixed-layer kaolinite-smectites is discussed. The authigenic origin of mixed-layer kaolinite‒smectite minerals in the studied sediments is substantiated.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"61 5","pages":"475 - 496"},"PeriodicalIF":0.7,"publicationDate":"2026-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148871521","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

Sulfides of the Copper‒Sulfur System as Indicators of the Conditions of Formation and Transformation of Cupriferous Sandstone and Shale Deposits 铜硫体系硫化物作为含铜砂岩和页岩矿床形成和转化条件的指示物

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2026-09-02 DOI: 10.1134/S0024490226600286

I. F. Gablina

{"title":"Sulfides of the Copper‒Sulfur System as Indicators of the Conditions of Formation and Transformation of Cupriferous Sandstone and Shale Deposits","authors":"I. F. Gablina","doi":"10.1134/S0024490226600286","DOIUrl":"10.1134/S0024490226600286","url":null,"abstract":"This paper examines cupriferous sandstones and shales hosted in sediments of varying ages (from P2 to PR2) and altered to different degrees (from early catagenesis to the epidote–amphibolite stage). The formation of these rocks is associated with the removal of Cu and other metals by formation waters from the red-colored ore-hosting rocks and their precipitation as sulfides on hydrosulfuric biogeochemical barriers. After their formation, cupriferous sandstones and shales can undergo metamorphic and supergene alterations, which are reflected in the crystallochemical properties of sulfide minerals, the composition of their paragenetic assemblages, the mineral zoning of mineralization, the morphology of ore bodies, and other features. This paper focuses on sulfides of the Cu—S system formed under various conditions. Their composition, structure, physicochemical and thermobaric stability, and occurrence in natural ores are discussed. The composition of copper sulfide ores in cupriferous sandstones, shales, and hypergenesis zones is elucidated. In particular, the paper explains why only nonstoichiometric Cu‒S sulfides (djurleite, geerite, spionkopite, yarrowite) are present in unaltered cupriferous sandstone ores and hypergenesis zones, whereas stoichiometric copper sulfides (chalcocite, digenite, and tetragonal phase) occur in metamorphosed ores. This fact is explained from a physical and chemical perspective. It has been established that each stage of rock formation and transformation is characterized by specific typomorphic minerals of the Cu‒S system and their parageneses that are stable under the conditions of a given stage. With increasing metamorphic grade, the mineral composition of ores and mineral zoning of the deposits change consistently toward simplification due to the gradual disappearance of low-temperature compounds and associations. Indicator minerals of the Cu‒S system, reflecting the thermobaric and chemical conditions of ore formation and transformation, have been identified.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"61 5","pages":"453 - 474"},"PeriodicalIF":0.7,"publicationDate":"2026-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148871817","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

Facies and Sequence Stratigraphy of the Zhuya Group in the Ura Uplift (Vendian, Southern Middle Siberia) 中西伯利亚南部文甸乌拉隆起朱雅群相层序地层学

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2026-09-02 DOI: 10.1134/S0024490226600249

S. V. Rud’ko, B. G. Pokrovsky, O. M. Silaeva

{"title":"Facies and Sequence Stratigraphy of the Zhuya Group in the Ura Uplift (Vendian, Southern Middle Siberia)","authors":"S. V. Rud’ko, B. G. Pokrovsky, O. M. Silaeva","doi":"10.1134/S0024490226600249","DOIUrl":"10.1134/S0024490226600249","url":null,"abstract":"The facies were studied and the sequence-stratigraphic model of the Zhuya Group in the Ura Uplift (Vendian reference section, southern area of Middle Siberia) was constructed. The whole Zhuya Group represents a single sequence bounded by unconformities. Sediments of the Kullekin member were accumulated in the high-energy coastal-marine environments during sea-level lowstand. The development of transgression initiated a carbonate ramp on the Siberian Craton. The rest of the Zhuya Group above the Kullekin member records the gradual progradation of the ramp and basin compensation of accommodation space during sea-level highstand. The trajectory of the negative C isotope excursion of the Zhuya Group, correlated with the Shuram–Wonoka excursion, follows the relative sea level changes, reaching its nadir close to the maximum of transgression. Elucidation of the reason for the coincidence of these trends requires additional regional and interregional studies. The occurrence of Neoproterozoic zircons in the Kullekin sandstones derived from a northern source reflects accretion of the Baikal–Muya terrane to the Siberian Platform and can be attributed to either pre-Zhuya inversion of the Patom basin (collision) or erosion of synsedimentary tuffs on the Siberian Platform (soft accretion).","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"61 5","pages":"542 - 556"},"PeriodicalIF":0.7,"publicationDate":"2026-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148871814","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

Mineralogical and Geochemical Features, Source Areas, and Formation Settings of Middle Permian Terrigenous Rocks of the Barabash Formation in Southwestern Primorye (Russia) 俄罗斯滨海地区西南部Barabash组中二叠统陆源岩的矿物学地球化学特征、源区及形成背景

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2026-09-02 DOI: 10.1134/S0024490226600262

A. I. Malinovsky

{"title":"Mineralogical and Geochemical Features, Source Areas, and Formation Settings of Middle Permian Terrigenous Rocks of the Barabash Formation in Southwestern Primorye (Russia)","authors":"A. I. Malinovsky","doi":"10.1134/S0024490226600262","DOIUrl":"10.1134/S0024490226600262","url":null,"abstract":"In the southwestern part of Primorye, the widespread Permian volcanosedimentary frocks are a part of the Paleozoic–Early Mesozoic Laoeling–Grodekovo terrane, a fragment of the eastern end of the Central Asian Foldbelt. The Middle Permian Barabash Formation is exposed fragmentarily in the southern part of the terrane, and the material composition of its terrigenous rocks is almost unstudied. The aim of the study was to investigate specific features of the material composition of sandy rocks of the Barabash Formation and, based on its interpretation, to identify paleogeodynamic environments of the formation of rocks, as well as to determine the composition and age of the sources of clastic material. The obtained results show that the sandstones (graywackes and, in part, lithic arenites) are petrogenic or “first cycle” rocks that underwent one cycle of redeposition, and they were deposited due to the destruction of moderately weathered rocks in source areas. A comprehensive analysis and paleogeodynamic interpretation of the mineralogical and geochemical composition of sandy rocks indicate that the rocks were deposited in a basin associated with an active continental margin environment and, in all likelihood, complicated by strike-slip dislocations along transform faults. The main source of clastic material was continental land – cratons and uplifted basement blocks composed of granite-metamorphic complexes and, in part, sedimentary rocks enriched with ancient clastic components. Additional source was fragments of an ancient, deeply eroded island arc composed of basic and ultramafic rocks. U–Pb dating of detrital zircon grains from sandstones of the Barabash Formation made it possible to determine the age of igneous rocks, which that served as the main sources of clastic material, and to reconstruct their probable location.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"61 5","pages":"497 - 514"},"PeriodicalIF":0.7,"publicationDate":"2026-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148871815","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

Th/U and Ti/Al Ratios in Upper Ediacaran Phosphorite-Bearing Mudstones of the Lviv–Kishinev Depression and Moscow Syneclise in the East European Platform 东欧地台Lviv-Kishinev坳陷和Moscow sysyise上埃迪卡拉统含磷泥岩Th/U和Ti/Al比值

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2026-07-02 DOI: 10.1134/S0024490226600171

S. B. Felitsyn

引用次数: 0

Specific Features of the Distribution Pattern of Detrital Zircon Age in the Epi-Hercynian Molasse of the Greater Caucasus (Lower Permian Aksaut Formation) 大高加索外延-海西期Molasse（下二叠统Aksaut组）碎屑锆石年龄分布模式的特征

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2026-07-02 DOI: 10.1134/S0024490226600158

A. S. Novikova, N. B. Kuznetsov, A. A. Razumovskiy, I. V. Fedyukin, T. V. Romanyuk, I. V. Latysheva, K. I. Dantsova, A. V. Shatsillo, O. A. Maslova, A. S. Dubenskiy, K. G. Erofeeva, V. S. Sheshukov

{"title":"Specific Features of the Distribution Pattern of Detrital Zircon Age in the Epi-Hercynian Molasse of the Greater Caucasus (Lower Permian Aksaut Formation)","authors":"A. S. Novikova, N. B. Kuznetsov, A. A. Razumovskiy, I. V. Fedyukin, T. V. Romanyuk, I. V. Latysheva, K. I. Dantsova, A. V. Shatsillo, O. A. Maslova, A. S. Dubenskiy, K. G. Erofeeva, V. S. Sheshukov","doi":"10.1134/S0024490226600158","DOIUrl":"10.1134/S0024490226600158","url":null,"abstract":"Results of the U‒Pb isotope dating of detrital zircon grains from sandstones in the typical section of the Lower Permian Aksaut Formation on the northern slope of the Greater Caucasus are presented. This formation represents a structural element of the Hercynian molasse that completes the Hercynide section in the Greater Caucasus. Results of the U‒Pb dating of detrital zircons from the Aksaut Formation sandstones are compared with the previously published similar data on metasedimentary rocks of various ages within the Hercynides of the Greater Caucasus, as well as with the date intervals of crystalline complexes that comprise the Hercynian basement of the Greater Caucasus. Prominent age peaks at about 309 and 385 Ma on the probability density curve characterizing the distribution of detrital zircon dates from sandstones of the Aksaut Formation are related to the widespread development of granite magmatism and metamorphism in the central part of the Greater Caucasus with dates closely corresponding to the above age peaks. The presence of numerous zircon groups with ages of 450‒750 Ma in the Aksaut sandstones is associated with: (1) erosion products of magmatic manifestations in the Cadomide blocks (peri-Gondwanan terranes) participating in the structure of Hercynides in the Greater Caucasus, (2) recycling detrital zircons from igneous complexes of the peri-Gondwanan terranes and/or rocks of Upper Precambrian and Lower Paleozoic sequences composed of erosion products of the peri-Gondwanan terranes into the Late Paleozoic Aksaut Formation rocks.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"61 4","pages":"384 - 409"},"PeriodicalIF":0.7,"publicationDate":"2026-07-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148366056","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

Causes, Mechanisms and Rates of Land Subsidence in the Red River Delta and Warnings of Excessive Groundwater Exploitation 红河三角洲地面沉降的原因、机制和速率及地下水过度开采的预警

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2026-07-02 DOI: 10.1134/S0024490226600146

Nghi Tran, Thu Trinh Hoai, Renat Shakirov, Natalia Sokolova, Huong Tran Thi Thuy, Nam Le Dinh, Toan Ngo Quang, Thanh Dinh Xuan, Nhuan Do Van, Thao Nguyen Thi Phuong, Anh Bui Thi Bao, Hang Pham Thi Thu, Tung Nguyen Xuan

{"title":"Causes, Mechanisms and Rates of Land Subsidence in the Red River Delta and Warnings of Excessive Groundwater Exploitation","authors":"Nghi Tran, Thu Trinh Hoai, Renat Shakirov, Natalia Sokolova, Huong Tran Thi Thuy, Nam Le Dinh, Toan Ngo Quang, Thanh Dinh Xuan, Nhuan Do Van, Thao Nguyen Thi Phuong, Anh Bui Thi Bao, Hang Pham Thi Thu, Tung Nguyen Xuan","doi":"10.1134/S0024490226600146","DOIUrl":"10.1134/S0024490226600146","url":null,"abstract":"Quaternary sediment subsidence in the Red River Delta has been quietly occurring for 1600 ka BP. This paper introduces the causes, mechanisms, and rates of tectonic subsidence and subsidence due to sediment compression in three boreholes selected for detailed study: BH4-HN, BH02-HP, and BH56-ND, representing three key areas of the Red River Delta. The activities of the northwest-southeast co-sedimentary fault systems and the northeast-southwest post-sedimentary fault systems have created a weak subsidence zone in Hanoi and two strong subsidence zones in Hai Phong and Nam Dinh. The results of sequence stratigraphy analysis show that these 3 boreholes all have 5 sequences: (1) ({text{Q}}_{1}^{1}): Early Pleistocene; (2) ({text{Q}}_{1}^{{2{text{a}}}}): Early middle Pleistocene; (3) ({text{Q}}_{1}^{{2{text{b}}}}): Late middle Pleistocene; (4) ({text{Q}}_{1}^{{3{text{a}}}}): Early late Pleistocene; (5) ({text{Q}}_{1}^{{3{text{b}}}})-Q2: Late late Pleistocene-Holocene. These 5 sequences are related to 5 glacial/interglacial cycles. Each sequence has 3 sedimentary systems tracts: lowstand (LST), transgressive (TST), and highstand (HST) systems tracts. The sequences and system tract of the 3 boreholes were calculated for the total of tectonic subsidence rate and sediment compression rate as follows: BH4-HN has Vav of 0.281 mm/year, BH02-HP: 0.63 mm/year, and BH56-ND: 0.799 mm/year. This has shown that the two strong subsidence zones of Hai Phong and Nam Dinh cause the strong estuaryization process at the Bach Dang estuary and the strong erosion of the Hai Hau coast.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"61 4","pages":"410 - 430"},"PeriodicalIF":0.7,"publicationDate":"2026-07-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148366055","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

Genesis of Sedimentary Fluorite in Light of Experimental Data 从实验资料看沉积萤石成因

IF 0.7 4区地球科学

Lithology and Mineral Resources Pub Date : 2026-07-02 DOI: 10.1134/S0024490226600183

A. V. Savenko, V. S. Savenko

{"title":"Genesis of Sedimentary Fluorite in Light of Experimental Data","authors":"A. V. Savenko, V. S. Savenko","doi":"10.1134/S0024490226600183","DOIUrl":"10.1134/S0024490226600183","url":null,"abstract":"Correspondence of the main hypotheses of the sedimentary fluorite genesis with the available experimental data is discussed. Data on the saturation degree of seawater and large continental water basins by CaF2 are summarized. It was established that the fluorite formation at the carbonate–gypsum stages of salinization in evaporite basins with purely marine nourishment is impossible, since this requires an additional supply of fluorine from external sources, exceeding the marine F contribution by at least 1.5–4 times. Authigenic fluorite can also form in arid continental water basins similar to the modern, greatly dried-up Aral Sea. It is shown that interaction of sedimentary carbonate minerals with the seawater leads to the dissolved F removal, which is more than an order of magnitude greater for dolomite than for calcite and aragonite. According to a new physicochemical mechanism proposed for the authigenic fluorite formation, recrystallization of the primary finely dispersed carbonate minerals with a defective crystalline structure (for example, protodolomite) promotes a partial self-purification of the solid phase from incoherent elements, accompanied by the accumulation of dissolved F in pore waters until the CaF2 saturation is achieved and fluorite is deposited.","PeriodicalId":18150,"journal":{"name":"Lithology and Mineral Resources","volume":"61 4","pages":"345 - 357"},"PeriodicalIF":0.7,"publicationDate":"2026-07-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148365880","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