Article
Geochemistry & Geophysics
Maryam Bendokht, Ali Reza Davoudian, Nahid Shabanian, John M. Cottle, Yunpeng Dong, Xiaoming Liu
Summary: Meta-granites in the Tutak metamorphic Complex preserve crucial information about the Late Neo-proterozoic tectonic history of the Sanandaj-Sirjan Zone, Iran. This paper employs comprehensive zircon U-Pb geochronology, whole-rock geochemistry, and zircon Lu-Hf isotopic data to elucidate the protolith, tectonic setting, and evolutionary history of these rocks. The results suggest that the granitic melts in the Sanandaj-Sirjan Zone were produced via partial melting of lower crustal igneous crustal rocks and sedimentary sources, and were formed in a post-collisional setting related to the convergence of peri-Gondwana terranes and Iranian continental fragments.
Article
Geochemistry & Geophysics
Masoumeh Zare-Shooli, Zahra Tahmasbi, Songjian Ao, Hua-Feng Zhang, Adel Saki, Ahmad Ahmadi-Khalaji, Chris Yakymchuk, Rasoul Esmaeili, Orhan Karsli
Summary: Migmatites in the Boroujerd region of Western Iran are associated with felsic and mafic magmatism, with the relationship between partial melting and magmatism being unclear. U-Pb zircon geochronology was used to determine the timing of anatexis in four metapelite migmatite samples. The detrital zircons in the migmatites correspond to the Paleozoic and Mesozoic magmatism in the region, while zircon rims and neoblastic grains suggest contact metamorphism and partial melting due to Middle Jurassic magmatism.
Article
Geosciences, Multidisciplinary
Zhong-Mei Wang, Chun-Ming Han, Wen-Jiao Xiao, Zhi-Yong Zhang
Summary: The Ghorveh batholith in Iran preserves sequences of Mesozoic plutonic and volcanic rocks. The granites in the southern part of the Ghorveh pluton have A-type granitic affinity and are derived from partial melting of crustal materials. The monzodiorites, on the other hand, have a mantle-derived origin. The development of the Ghorveh area was a result of subduction and back-arc extension during the Late Jurassic.
GEOLOGICAL JOURNAL
(2023)
Article
Geochemistry & Geophysics
Makiko K. Haba, Joern-Frederik Wotzlaw
Summary: Eucrite meteorites are believed to originate from the upper crust of the asteroid Vesta, with zircons providing insight into the initial magmatism and thermal metamorphism that occurred around 4550-4555 million years ago on Vesta. By using advanced dating methods, researchers were able to distinguish zircons formed during different thermal events in the early stages of Vesta's crustal evolution, shedding light on the formation and history of the Vesta crust. The findings suggest that zircons in eucrites like Camel Donga were formed during early magmatism or global thermal metamorphism in the early stages of Vesta's crustal formation.
Article
Geosciences, Multidisciplinary
Farzaneh Shakerardakani, Franz Neubauer, Xiaoming Liu, Yunpeng Dong, Behzad Monfaredi, Xian-Hua Li
Summary: The new detrital U-Pb zircon ages from the Sanandaj-Sirjan metamorphic zone provide insights into the late Neoproterozoic to early Palaeozoic plate tectonic evolution. The most abundant detrital zircon population includes Ediacaran ages, with other significant age peaks identified. The sediment sources may be from within the Iranian microcontinent or from elsewhere.
GEOLOGICAL MAGAZINE
(2021)
Review
Geosciences, Multidisciplinary
Tiantian Wang, Jahandar Ramezani, Chuan Yang, Jianghai Yang, Qiong Wu, Zhihui Zhang, Dawei Lv, Chengshan Wang
Summary: Sedimentary rocks are important repositories of Earth history, and the U-Pb radioisotopic system is a precise and accurate method for measuring absolute time. However, its application to the stratigraphic record relies on the presence of relatively pure volcanic ash deposits. Innovations in U-Pb ID-TIMS geochronology have improved precision and reproducibility, but have also revealed complexities in the U-Pb systematics of minerals.
EARTH-SCIENCE REVIEWS
(2023)
Article
Geochemistry & Geophysics
Sean P. Gaynor, Melissa Ruiz, Urs Schaltegger
Summary: This study presents high-precision isotope dilution-thermal ionization mass spectrometry (ID-TIMS) U-Pb zircon data from the Carboniferous Punteglias granodiorite in Switzerland. The results show that the zircon crystals have a mixture of two different age components, and the crystallization age of the zircon is determined to be 335.479 +/- 0.041 Ma. Additionally, pretreating the zircon samples with physical and chemical abrasion reduces age dispersion and allows for a more accurate determination of the initial magmatic domains. The high analytical precision of this study is crucial for correctly interpreting complex age spectra.
Article
Geosciences, Multidisciplinary
Maryam Bendokht, Nahid Shabanian, Ali Reza Davoudian, Yunpeng Dong, John M. Cottle, T. Alexander Johnson
Summary: A study on Cadomian orthogneisses from the Tutak metamorphic complex in Iran reveals an Early Cambrian crystallization age and indicates derivation in a subduction zone environment. Isotopic data suggest a metasomatic lithospheric mantle source with a crustal component contributed via partial melting of metabasite.
PRECAMBRIAN RESEARCH
(2021)
Review
Geochemistry & Geophysics
Reza Maghdour-Mashhour, Ben Hayes, Kwan-Nang Pang, Robert Bolhar, Amir Ali Tabbakh Shabani, Fatima Elahi-Janatmakan
Summary: The Zagros suture zone in Iran is part of the Tethyan orogenic belt that records convergence between the Eurasian and Arabian plates during the Mesozoic-Cenozoic. The study reviews geological information relevant to the Sanandaj-Sirjan zone, emphasizing Jurassic igneous activity, and proposes two episodes of orogenesis based on existing geochemical data. The research suggests that subduction zone initiation in the Sanandaj-Sirjan zone was episodic and involved periods of subduction and trench retreat interrupted by short-lived contraction events.
Article
Geosciences, Multidisciplinary
Neda Tavakoli, Nahid Shabanian, Ali Reza Davoudian, Hossein Azizi, Franz Neubauer, Yoshihiro Asahara, Manfred Bernroider, James K. W. Lee
Summary: The Boein-Miandasht Complex in western Iran is composed of various rocks formed in the Late Jurassic, displaying typical characteristics of ferroan A-type granites. The formation of these rocks may be attributed to extensional tectonic regime and partial melting of the lower crust due to the injection of hot mafic magmas within the crust.
JOURNAL OF ASIAN EARTH SCIENCES
(2021)
Article
Geochemistry & Geophysics
Abdolnaser Fazlnia, Kwan-Nang Pang, Wei-Qiang Ji
Summary: The Cretaceous Gharuchah-Sofla intrusion in Iran is a composite batholith consisting of various mafic to felsic rocks. The age and relationships between different rock types in the intrusion were unknown. Through detailed studies, it was found that the intrusion was dominated by Early Cretaceous and Ediacaran magmatic rocks, characterized by sub-alkaline compositions. The formation of these rocks was likely associated with Cadomian basement melting and fractional crystallization processes.
Article
Geology
Alireza Zarasvandi, Mohsen Rezaei, Johann G. Raith, David R. Lentz
Summary: The study revealed that granitoid intrusions in the Zagros orogenic belt exhibit different geological features at different geological times, with the Cenozoic intrusions being more hydrous and oxidized, which facilitated the formation of mineral deposits.
INTERNATIONAL GEOLOGY REVIEW
(2022)
Article
Geology
Fatemeh Nouri, Robert J. Stern, Hossein Azizi
Summary: The northern Sanandaj-Sirjan Zone in western Iran is an important province for semi-gemstone deposits of tourmaline, beryl, and garnet associated with Jurassic granites. The deposits belong to six different types and have complex geological origins.
INTERNATIONAL GEOLOGY REVIEW
(2022)
Article
Geosciences, Multidisciplinary
Liangliang Zhuang, Yucai Song, David Leach, Yingchao Liu, Zengqian Hou, Mahmood Fard
Summary: The Angouran deposit is the second-largest Zn-Pb deposit in Iran, hosting sulfide mineralization in a marble-schist sequence within a breccia pipe in a domal structure. The features of the ore-hosting breccias resemble known halokinetic diapir breccias, with subtle evaporite minerals.
GEOLOGICAL SOCIETY OF AMERICA BULLETIN
(2023)
Article
Geology
Narges Daneshvar, Mohammad Maanijou, David R. Lentz, Hossein Azizi, Chris R. M. McFarlane, Teruyuki Maruoka
Summary: The Qolqoleh gold deposit in northwest Iran contains four generations of Au-bearing sulfides, with element compositions indicating the multistage role of hydrothermal systems and an early hydrothermal event related to magmatic fluids from the Carboniferous period.
ORE GEOLOGY REVIEWS
(2021)
Article
Geosciences, Multidisciplinary
Hadi Shafaii Moghadam, Fernando Corfu, Robert J. Stern, Ali Lotfi Bakhsh
JOURNAL OF THE GEOLOGICAL SOCIETY
(2019)
Article
Geosciences, Multidisciplinary
Jiri Konopasek, Robert Anczkiewicz, Petr Jerabek, Fernando Corfu, Eliska Zackova
JOURNAL OF THE GEOLOGICAL SOCIETY
(2019)
Article
Geochemistry & Geophysics
Alexei V. Ivanov, Ivan V. Levitskii, Valery I. Levitskii, Fernando Corfu, Elena I. Demonterova, Leonid Z. Reznitskii, Ludmila A. Pavlova, Vadim S. Kamenetsky, Valery M. Savatenkov, Vladislav I. Powerman
Article
Geochemistry & Geophysics
Hans Jorgen Kjoll, Torgeir B. Andersen, Fernando Corfu, Loic Labrousse, Christian Tegner, Mohamed Mansour Abdelmalak, Sverre Planke
Article
Geosciences, Multidisciplinary
F. Corfu, M. Heim
JOURNAL OF THE GEOLOGICAL SOCIETY
(2020)
Article
Geochemistry & Geophysics
Bjorn Jamtveit, Arianne Petley-Ragan, Sarah Incel, Kristina G. Dunkel, Claire Aupart, Hakon Austrheim, Fernando Corfu, Luca Menegon, Francois Renard
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2019)
Article
Geochemistry & Geophysics
Bahman Rahimzadeh, Shahryar Mahmoudi, Fernando Corfu, Vahid Ahadnejad, Albrecht Von Quadt
Summary: The Sanandaj-Sirjan metamorphic-magmatic Zone (SaSZ) is the Mesozoic active continental margin between the Arabian plate and the Iranian plateau. It evolved at the margin of ancient Ediacaran basement, with an age of 557 Ma for a trondhjemite. The Mesozoic activity of the SaSZ was most intense in the Jurassic period between 170 and 150 Ma.
Article
Geosciences, Multidisciplinary
Shahryar Mahmoudi, Fernando Corfu
Summary: The composite Poshteh Pluton in eastern Iran is located at a critical tectonic junction and is part of the Central Iranian Microplate. It consists of two distinct intrusions and is positioned south of the inferred main Paleotethys suture and along the Doruneh Fault system. The quartz monzonite in the Pluton has been dated to 215.8 +/- 0.5 Ma, which coincides with the closure of the Paleotethys during the late stages of the Eo-Cimmerian Orogeny. It is similar to coeval plutons along the Paleotethys suture and likely formed through disruption processes during the Mesozoic and Cenozoic. The Pluton was subsequently invaded by granite at 41.23 +/- 0.31 Ma, associated with structural control and hydrothermal alteration. This granite is part of a late Eocene to Oligocene plutonic suite in the region and formed through subcontinental lithosphere delamination and melting.
INTERNATIONAL JOURNAL OF EARTH SCIENCES
(2022)
Article
Geosciences, Multidisciplinary
Kenneth Warvik, Hakon Blaker Ringstad, Lars E. Augland, Fernando Corfu, Roy H. Gabrielsen
Summary: The Caledonian Orogen preserves the complete record of a Wilson cycle, and Revsegg Allochthon is an understudied example in the southern Scandinavian Caledonides that illustrates the key temporal and tectonic stages in the cycle.
JOURNAL OF THE GEOLOGICAL SOCIETY
(2022)
Article
Geosciences, Multidisciplinary
Fernando Corfu, Torgeir B. Andersen
Summary: The break-up of continents can lead to the formation of dyke swarms, basins, and hyperextension assemblages. The Nalfjell Complex in northern Norway has the characteristics of a hyperextension assemblage, including serpentinite bodies embedded in various rocks. The ages and evolution of the Nalfjell Complex differ from other structural units in the region.
JOURNAL OF THE GEOLOGICAL SOCIETY
(2022)
Article
Geochemistry & Geophysics
Ariela Mazoz, Guilherme O. Goncalves, Cristiano Lana, Ian S. Buick, Fernando Corfu, Sandra L. Kamo, Hao Wang, Yue-Heng Yang, Ricardo Scholz, Glaucia Queiroga, Bin Fu, Lorena Martins, Mathias Schannor, Adriana Tropia de Abreu, Marly Babinski, Eliza Peixoto, Roberto Ventura Santos
Summary: The Khan River and Bear Lake titanites were investigated as potential reference materials for LAICP-MS applications. Both titanites showed consistent U-Pb and Nd-isotope ratios, but the Khan River titanite exhibited heterogeneity in texture and composition.
GEOSTANDARDS AND GEOANALYTICAL RESEARCH
(2022)
Article
Geosciences, Multidisciplinary
Tor Grenne, Deta Gasser, Reidulv Boe, Fernando Corfu, Oyvind Skar, Trond Slagstad
Summary: This study presents a revised stratigraphic and tectonomagmatic model for the Holonda area, based on remapping, sedimentology, igneous geochemistry, isotopes, and geochronology. The findings suggest that the region experienced arc-continent collision, subduction polarity flip, and rifting, leading to the opening of a wide basin. The study provides valuable insights into the Caledonian orogen and the central Mediterranean tectonic models.
JOURNAL OF THE GEOLOGICAL SOCIETY
(2023)
Article
Geosciences, Multidisciplinary
Sascha Zertani, Luca Menegon, Giorgio Pennacchioni, Iris Buisman, Fernando Corfu, Bj orn Jamtveit
Summary: Deformation of the continental crust is influenced by various factors, including pre-existing structural framework, fluid availability, strain rate, and pressure-temperature conditions. By investigating the evolution of a large shear zone in Lofoten, Norway, we found that deformation occurred through multiple metamorphic stages and mechanical heterogeneities influenced the deformation style and fluid channelization.
JOURNAL OF STRUCTURAL GEOLOGY
(2023)
Article
Geochemistry & Geophysics
Ariela Mazoz, Guilherme O. Goncalves, Cristiano Lana, Ian S. Buick, Fernando Corfu, Sandra L. Kamo, Hao Wang, Yue-Heng Yang, Ricardo Scholz, Gloucia Queiroga, Bin Fu, Lorena Martins, Mathias Schannor, Adriana Tropia de Abreu, Marly Babinski, Eliza Peixoto, Roberto Ventura Santos
Summary: The titanites from Khan River and Bear Lake were investigated as potential reference materials for LA-ICP-MS applications. Both titanites showed consistent U-Pb and Nd-isotope ratios, making them suitable for Nd-isotope analyses.
GEOSTANDARDS AND GEOANALYTICAL RESEARCH
(2022)
Review
Geosciences, Multidisciplinary
Fuquan Yang, Xinxia Geng, Zhixin Zhang, Guoren Liu, Hanqing Zhang
Summary: Northern Xinjiang in China is an important part of the Central Asian Orogenic Belt, characterized by multiple episodes and types of mineralization. Cu and Au deposits are mostly found in Altay, Junggar, and Tianshan, with minor occurrences in Beishan. The most common types of Cu-Au deposits are volcanogenic and porphyry deposits. The formation of Cu-Au deposits can be divided into five mineralization episodes, with the Devonian and Carboniferous being the main periods. These deposits developed in various tectonic settings, including island arc, continental arc, collision, and postcollisional extensional tectonics.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Jiang Zhu, Dan-yang Liu, Chao Chen, Song Chen, Yuan-bing Zou, Leonid Danyushevsky, Jing-meng Huang, Xiang-wei Tang
Summary: Numerous lode gold and silver deposits have been discovered in orogenic belts in China. This study focuses on the formation and fluid evolutions of the super-large Yingdongpo gold and giant Poshan silver deposits in the Tongbai-Dabie orogen. The results suggest that both deposits were formed concurrently with Early Cretaceous granitic magmatism and the ore-forming fluids were primarily of magmatic origin with meteoric water inputting. The gold mineralization is related to a change in the physicochemical properties of the fluids, while the silver mineralization is favored by progressive deposition of sulfides in a slowly cooling hydrothermal system.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Arun Bhadran, B. P. Duarah, Drishya Girishbai, Mohammad Atif Raza, Avi Mero, Sandeep Lahon, A. L. Achu, Girish Gopinath
Summary: The Brahmaputra foreland basin, known for its dynamic tectonism and sediment load, exhibits a variety of seismically generated soft sediment deformation structures (SSDS) such as clastic dikes, sand sills, and micro-faults. These structures, influenced by multiple strong seismic events, are characterized by their dimensions, intrusion angles, cross-cutting relations, wall shattering, and age. The study suggests that a significant earthquake with high intensity and magnitude might have caused liquefaction features in the area. The findings highlight the importance of studying SSDS in tectonically active regions with limited surface ruptures and dense alluvial cover.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Huan Wang, Lirong Dou, Xingyang Zhang, Jiquan Yin, Beiwei Luo, Haigang Duan, Peiguang Yang, Yifan Song
Summary: Quantitative analysis of sediment composition and microfacies helped identify changes in facies belts in the Cretaceous Mishrif Formation. The study demonstrated the importance of carbonate microfacies quantification and its implications for paleogeographic research.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Boran Wang, Zhilong Huang, Dongsheng Xiao, Haiyue Yu, Wenren Zeng, Xin Wang, Tong Qu, Zhiyuan Li, Yizhuo Yang
Summary: By systematically analyzing the source rocks of the Sangonghe Formation in the Taibei Sag, NW China, and using kerogen kinetics modeling, this study reveals the influence of geological conditions on hydrocarbon generation and expulsion. The source rocks in different environments show distinct geochemical characteristics and hydrocarbon generation potential.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Haiying Yang, Zhifang Zhao, Haifeng Fan, Min Zeng, Jiafei Xiao, Xiqiang Liu, Shengwei Wu, Jiangqin Chao, Yong Xia
Summary: This paper investigates the REE enrichment and the role of Fe/Mn (oxyhydr)oxides in marine phosphorites from the early Cambrian period in South China. The study reveals that Fe/Mn (oxyhydr)oxides play a crucial role in REE enrichment and are controlled by Fe-redox pumping.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Qing Li, Hongbin Wang, Feng Cai, Di Luo, Fanxing Kong, Ang Li, Xiting Liu
Summary: The elemental and isotopic compositions and abundance of carbonates in marine sediments are used to reconstruct ancient climate and ocean conditions. This study analyzed sediment samples from the Okinawa Trough to examine the relationship between carbonates' compositions and methane seepage and sea-level changes. The results indicate that both biogenic and authigenic carbonates are important factors in understanding paleoclimate and paleoceanography.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Maryam Akbarzadeh Aghdam, Abdolreza Ghods, Farhad Sobouti, Khalil Motaghi, Keith Priestley, Mohammad Enayat
Summary: The Makran subduction zone is difficult to monitor due to limited seismic activity, but a temporary seismic network was installed to investigate the relationship between different regions and detect seismicity. The observed seismicity suggests the presence of structural boundaries and seismically inactive areas.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Zhen-Yu Wang, Hong-Rui Fan, Hai-Dong She, Kui-Feng Yang
Summary: This study conducted detailed geochemical, geochronological and isotopic analyses on the Songxian syenite in the Qinling Orogen. The results revealed the magma sources, petrogenesis and geodynamic implications of this alkaline intrusion. The study suggests that the syenite was formed through multiple stages of magmatism, involving the partial melting of the enriched lithospheric mantle and mixing with melts derived from the lower crust.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Yu Li, Wen-Liang Xu, Xiao-Ming Zhang, Jie Tang
Summary: This study presents new zircon U-Pb-Hf and whole-rock geochemical data for Jurassic intrusive rocks in the Yanbian area of NE China, providing insights into the subduction history of the Paleo-Pacific Plate. The study reveals three stages of Jurassic magmatism in the area, indicating the presence of an active continental margin related to the initial subduction of the Paleo-Pacific Plate beneath the Eurasian continent.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Lina Ai, Shengfa Liu, Shuai Cong, Hui Zhang, Peng Cao, Kaikai Wu, Wenxing Ye, Che Abd Rahim Mohamed, Xuefa Shi
Summary: This study investigates the depositional configurations and sedimentary environments of the Malacca Strait through analyzing grain size characteristics and hydrographic data. The results show that residual sediments are concentrated in the central region, while modern terrigenous sediments are distributed along the coast of Malaysia and the northern region. The sedimentary environments are influenced by seasonal variations and hydrodynamic conditions.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Liang Xiao, Jia-qi Liang, Li-yan Guo, De-shuang Ji, Man Yuan, Xiang-chuan Li, Nan Sun, Zuo-chen Li
Summary: This study investigates the correlation between stable carbon isotopes of plant fossils and CO2 levels in the Jurassic period. The results suggest a weak correlation between the two, indicating caution is needed when using stable carbon isotopes to reconstruct high paleo-CO2 concentrations.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Xuli Yang, Feng Huang, Jifeng Xu, Xijun Liu, Liying Zhang, Zhao Zhang, Benyan Xu, Man Zhang, Yunchuan Zeng, Qian Liu, Mingda Lv
Summary: The extensively developed Early Cretaceous intermediate-felsic rocks in the northern North China Craton provide valuable insights into the nature of Paleo-Pacific subduction and associated geodynamic processes. Geochemical and geochronological analyses of trachyandesites and rhyolites from the eastern Hebei, northern NCC suggest that the trachyandesites likely originated from enriched mafic lower crust and the rhyolites are derived from the trachyandesitic magmas through fractional crystallization. The migration direction change of these rocks is believed to be primarily attributed to slab rollback of the subducting Paleo-Pacific Plate.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Wei Liu, Ping Gao, Xianming Xiao, Yanming Zhao, Yijie Xing, Jinku Li
Summary: The organic-rich shales of the Shuijingtuo Formation in China are an important target for shale gas exploration. The upper section of the formation, primarily consisting of limestone, silty shale, and black shale, has been rarely studied but recently showed promising results for shale gas exploration. Geochemical investigations of the upper section shale deposits revealed that the organic matter enrichment mechanism underwent dynamic changes due to relative sea-level changes and episodic upwelling activities.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
Article
Geosciences, Multidisciplinary
Xin Wang, Chen Zhang, Zixin Xue, Qianyou Wang, Zhenxue Jiang, Kun Zhang, Xiangye Kong
Summary: This study analyzed the heterogeneity of gas compositions and the effects of magmatism on gas accumulation in shale gas exploration in the Yangtze plate. The results showed that magmatism caused the development of micro-fractures in shale reservoirs and accelerated the thermal evolution rate of organic matter. The impact of magmatism on shale gas accumulation varied in different regions, either favoring or compromising efficient gas accumulation in shale reservoirs.
JOURNAL OF ASIAN EARTH SCIENCES
(2024)
