Article
Geosciences, Multidisciplinary
Yongfei Zheng, Yixiang Chen, Renxu Chen, Liqun Dai
Summary: This article discusses the changes in the dynamic regime and geothermal gradient of subduction zones at convergent plate boundaries in different stages, as well as the types of metamorphism and magmatism associated with them. These studies are of great significance for understanding the tectonic evolution of the Earth and the formation of rocks.
SCIENCE CHINA-EARTH SCIENCES
(2022)
Article
Geochemistry & Geophysics
M. Ersen Aksoy, Mustapha Meghraoui, Alina Polonia, M. Namik Cagatay, Asli Zeynep Yavuzoglu, Sebnem Onder, Umut B. Ulgen, Luca Gasperini
Summary: This study focused on the westernmost segment of the North Anatolian fault in NW Turkey and found that the western termination of the 1912 earthquakes' surface ruptures ends about 37 km offshore in the Gulf of Saros. The research suggests that the eastern extension of the 9 August earthquake reached the Central Marmara Basin, with implications for seismic hazard in the Marmara coastal area.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2022)
Article
Geosciences, Multidisciplinary
M. Wildman, R. Brown, J. Ye, D. Chardon, D. Rouby, A. N. Kouamelan, M. Dall'Asta
Summary: This study investigates the thermal and tectonic evolution of the West African continental margins through new apatite fission-track (AFT) data analysis in Guinea and Ivory Coast. The results reveal the thermal effect of the Central Atlantic Magmatic Province (CAMP), rapid cooling along the coast during the early to mid-Cretaceous period, and moderate cooling across longer wavelengths.
Article
Geochemistry & Geophysics
M. Rodriguez, D. Sakellariou, C. Gorini, A. Janin, E. D'Acremont, L. Le Pourhiet, N. Chamot-Rooke, K. Tsampouraki-Kraounaki, I Morfis, G. Rousakis, P. Henry, A. Lurin, M. Delescluse, P. Briole, A. Rigo, S. Arsenikos, C. Bulois, D. Fernandez-Blanco, A. Beniest, C. Grall, F. Chanier, F. Caroir, J-X Dessa, D. Oregioni, A. Nercessian
Summary: This study uses seismic reflection lines to reveal the subsurface structure and sedimentary record in the North Aegean region, and finds that the two main branches of the North Anatolian Fault were formed 1.3-2 million years ago, and since the Early Pleistocene, the North Aegean Troughs have been propagating westwards to form horsetail basins.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2023)
Article
Geochemistry & Geophysics
Tae-Kyung Hong, Junhyung Lee, Jeongin Lee, Seongjun Park, Byeongwoo Kim, Sungchan Choi
Summary: Earthquakes in the Korean Peninsula often occur in subsurface hidden faults that are difficult to identify before seismic activity. In this study, a midcrustal subsurface hidden fault in a seismically quiet region of the central Korean Peninsula was investigated, which caused the M-L 4.1 earthquake on October 28, 2022. Combined analysis of seismicity, geophysical properties, and geological features provided constraints on the geometry of this hidden fault. The fault extends to the surface where a lineament with low gravity anomalies is present.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2023)
Article
Geochemistry & Geophysics
Yanchuan Li, Jean-Mathieu Nocquet, Xinjian Shan
Summary: This study combines GPS velocity field with InSAR results to investigate the interseismic deformation of the western Altyn Tagh fault (ATF) at longitude 86 degrees E. The findings show the presence of sinistral shear and NS shortening near the Manyi fault system, while the slip rate and locking depth across the ATF are relatively lower. Additionally, no significant offset between the surface fault trace and the fault at depth is observed, suggesting no lateral variations of the elastic strength across the ATF.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2022)
Article
Geochemistry & Geophysics
Yanchuan Li, Jean-Mathieu Nocquet, Xinjian Shan
Summary: By combining GPS velocity field with InSAR results, this study investigates interseismic deformation across the western Altyn Tagh fault (ATF) and identifies a sinistral shear and NS shortening area near the Manyi fault system. The research highlights how different data sets, data selection, and model assumptions can impact results on ATF slip rate, locking depth, and rheological contrast across the fault.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2021)
Editorial Material
Geosciences, Multidisciplinary
Tiago M. Alves, Julie Tugend, Simon Holford, Claudia Bertoni, Wei Li
Summary: The geological processes responsible for the formation of continental margins are complex and vary between different margins and adjacent sedimentary basins. Understanding these processes is crucial for determining the economic potential of continental margins.
MARINE AND PETROLEUM GEOLOGY
(2021)
Article
Geochemistry & Geophysics
S. Rost, G. A. Houseman, A. W. Frederiksen, D. G. Cornwell, M. Kahraman, S. Altuncu Poyraz, U. M. Teoman, D. A. Thompson, N. Turkelli, L. Gulen, M. Utkucu, T. J. Wright
Summary: Research using dense seismic data reveals the subsurface structure of the North Anatolian Fault Zone, with findings showing lateral incoherence of crustal interfaces, contrasting crustal structures on either side of the fault zone, and strong variations in structure both north-south and east-west within the study region. The results suggest the presence of major shear zones throughout the crust and into the lithospheric mantle beneath the fault zone, indicating a strong coupling of strain at these depths.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2021)
Article
Geosciences, Multidisciplinary
Qing Bian, Shang Deng, Huixi Lin, Jun Han
Summary: The connection between source rock and reservoir separated by salt strata is a global problem. This paper focuses on the No. 5 strike-slip fault passing through salt layers in the Tarim Basin. The seismic data reveals different structural styles in the salt layer, including transpression, transtension, and pure strikeslip. The impact of deep strike-slip salt tectonics on petroleum exploration is discussed using data from seven wells, showing that thicker salt layers result in poorer production.
MARINE AND PETROLEUM GEOLOGY
(2022)
Article
Geology
Rodrigo J. J. Suarez, Miguel E. E. Ramos, Christian Sue, Matias Ghiglione, Vanesa Barberon, Paulo Quezada, Sandrine Roy
Summary: Based on a compilation of strain/stress tensors and evidence of syntectonic strata, combined with a seismotectonic appraisal, typical features of faulting in the Patagonian Andes are assessed. The prevalence of strike-slip faulting challenges the classic proposal for alternating extensional and contractional deformation phases in the Andean orogen. Strain partitioning and non-partitioned contexts are suggested as explanations for the Cenozoic patterns of deformation in the North and South Patagonian Andes respectively.
INTERNATIONAL GEOLOGY REVIEW
(2023)
Article
Geosciences, Multidisciplinary
Riccardo De Ritis, Massimo Chiappini
Summary: This paper presents a new high-resolution magnetic anomaly map of the La Fossa Caldera system and Lipari island in Southern Italy. The study identifies different magnetic anomalies in these islands, indicating diverse geological features. The magnetic anomalies in La Fossa Caldera are related to mafic intrusive/effusive sources, while those in Lipari island are related to sources with more evolved chemistry. The insights obtained from this study contribute to a better understanding of the relationship between arc volcanism and tectonics, and can help in forecasting future eruptions.
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH
(2023)
Article
Geochemistry & Geophysics
P. Papadimitriou, V Kapetanidis, A. Karakonstantis, I Spingos, K. Pavlou, G. Kaviris, I Kassaras, V Sakkas, N. Voulgaris
Summary: The characteristics of the M-w = 6.7 earthquake that occurred near Zakynthos Island, Greece in October 2018 were thoroughly examined, revealing strong spatial clustering of aftershocks in the northern and southern regions, potentially related to plate tectonics.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2021)
Article
Geochemistry & Geophysics
Tahir Serkan Irmak, Seda Yolsal-Cevikbilen, Tuna Eken, Bulent Dogan, Ceyhun Erman, Evrim Yavuz, Hakan Alcik, Peter Gaebler, Ali Pinar, Tuncay Taymaz
Summary: The study investigates the source properties, aftershock behavior, and coseismic deformation of the 2019 earthquake in the Central Marmara Sea region, indicating that secondary structures play a key role in the crustal kinematics of the area and are likely responsible for the main shock activity.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2021)
Article
Geochemistry & Geophysics
Lejun Lu, Yu Zhou
Summary: This study presents new geodetic observations of the 1976 Chaldiran earthquake in eastern Turkey, using historical KH imagery and modern Pleiades stereo imagery. The analysis reveals that the coseismic slip at the Hidirmentes segment is around 4.0 m, larger than the surface displacement of 3 m. This suggests that the earthquake deformation is a combination of slip on the primary fault and off-fault deformation. The study also finds a constant ratio of horizontal to vertical offsets, indicating characteristic slip behavior of the Chaldiran fault in the late Quaternary.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2023)
Article
Chemistry, Applied
Sara Marchionni, Antonella Buccianti, Andrea Bollati, Eleonora Braschi, Francesca Cifelli, Paola Molin, Maurizio Parotto, Massimo Mattei, Simone Tommasini, Sandro Conticelli
Article
Geosciences, Multidisciplinary
J. Ghalamghash, S. Z. Mousavi, J. Hassanzadeh, A. K. Schmitt
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH
(2016)
Article
Geosciences, Multidisciplinary
Badieh Shahsavari Alavijeh, Nematollah Rashidnejad-Omran, Fatma Toksoy-Koksal, Wenliang Xu, Jalil Ghalamghash
GEOSCIENCE FRONTIERS
(2019)
Article
Geosciences, Multidisciplinary
Badieh Shahsavari Alavijeh, Nematollah Rashidnejad-Omran, Fatma Toksoy-Koksal, David Chew, Krzysztof Szopa, Jalil Ghalamghash, Aleksandra Gaweda
GEOLOGICAL JOURNAL
(2019)
Article
Geosciences, Multidisciplinary
J. Ghalamghash, A. K. Schmitt, K. Shiaian, R. Jamal, Sun-Lin Chung
JOURNAL OF ASIAN EARTH SCIENCES
(2019)
Article
Geochemistry & Geophysics
J. Ghalamghash, A. K. Schmitt, R. Chaharlang
Article
Geochemistry & Geophysics
Massimo Mattei, Francesca Cifelli, Habib Alimohammadian, Hamideh Rashid
Article
Geochemistry & Geophysics
Razieh Chaharlang, Mihai N. Ducea, Jalil Ghalamghash
Article
Geosciences, Multidisciplinary
Vincenzo Amato, Pietro P. C. Aucelli, Massimo Cesarano, Carmen M. Rosskopf, Francesca Cifelli, Massimo Mattei
Summary: The Boiano Basin, located in the central-southern Apennines, is one of the largest Quaternary intermontane basins in the Mediterranean region. The filling of the basin began in the late Early Pleistocene and evolved with variations in lithofacies distribution and thickness. The Quaternary infilling is hypothesized to have occurred within a graben or semigraben structure, mainly affected by extensional fault systems in the inner part of the basin.
GEOLOGICAL JOURNAL
(2021)
Article
Geosciences, Multidisciplinary
Shahrouz Babazadeh, Massimo D'Antonio, John M. Cottle, Jalil Ghalamghash, Davood Raeisi, Yajun An
Summary: This study investigates the petrogenesis of high-alumina basalts (HABs) in the Cenozoic Eshtehard, revealing that these rocks are derived from the hydrated, depleted asthenospheric mantle wedge overlying subducted oceanic lithosphere. The rocks show enrichment in incompatible trace elements and homogeneous Sr-Nd isotopes, with a primary melt forming due to assimilation of crustal material while fractionating plagioclase, high Ca pyroxene, magnetite, and amphibole. Water content, sediment melt, and continental crust materials are suggested as key components in the generation of Eshtehard HABs.
Article
Geochemistry & Geophysics
Shahrouz Babazadeh, Jalil Ghalamghash, Massimo D'Antonio, Tanya Furman
Summary: The study in the Eshtehard area of Iran utilized volcanic materials to investigate the nature and effects of hydrothermal alteration, revealing significant changes in element abundances and whole rock geochemistry among different alteration facies. The presence of consistent negative Ce and Eu anomalies suggests reducing conditions during hydrothermal processes, while variations in isovalent element ratios imply non-charge and radius control behavior. Additionally, the slight REE tetrad effect observed in altered samples may be attributed to fluid-rock interaction in open system conditions. Fluid inclusions studies indicated boiling during mineralization, with ore forming fluids likely having a magmatic source and undergoing boiling and/or exchange with hydrous minerals.
JOURNAL OF GEOCHEMICAL EXPLORATION
(2021)
Article
Geosciences, Multidisciplinary
Shahrouz Babazadeh, Jalil Ghalamghash, Tanya Furman, Massimo D'Antonio, Davood Raeisi
Summary: The Avaj Oligocene volcanic-plutonic complex in Iran is studied using whole rock geochemistry, mineral compositions and crystal size distributions to determine the petrogenesis of the rocks. Findings suggest minor crustal assimilation occurred during magma ascent and longer magma residence time for plagioclase in plutonic samples compared to basaltic samples.
JOURNAL OF ASIAN EARTH SCIENCES
(2021)
Article
Geochemistry & Geophysics
Andrea Zanchi, Stefano Zanchetta, Fabrizio Berra, Massimo Mattei, Hamid Reza Javadi, Chiara Montemagni
Summary: This contribution demonstrates the pre-Miocene dextral activity of the Great Kavir - Doruneh Fault System (GKDFS) in Central Iran, with the Arusan Fault System (AFS) showing important dextral shearing. The study indicates that deformation occurred in a total simple shear regime, with enormous Meso-Cenozoic dextral displacements along the AFS and GKDFS attested by significant offsets of the Paleotethys suture zone.
Article
Geosciences, Multidisciplinary
Razieh Chaharlang, Jalil Ghalamghash, Yu Saitoh, Mihai N. N. Ducea, Axel K. K. Schmitt
Summary: Late Miocene-Quaternary adakitic rocks are widely distributed in northwestern Iran and are believed to have formed after a slab break-off event at around 10 million years ago. The Sabalan adakitic rocks in northwest Iran show near-identical Sr-Nd isotopic characteristics, indicating that they were mainly generated by melting of juvenile intrusions in the lower crust. The delay between the slab break-off and magmatic activity suggests that the melting was triggered by asthenospheric melting underneath the Turkish-Iranian Plateau. It is proposed that the detached slab heated up in the mantle, causing dehydration and subsequent ascent of fluids that lowered the mantle viscosity, leading to partial melting of lower crustal rocks and the generation of adakitic magmas.
INTERNATIONAL JOURNAL OF EARTH SCIENCES
(2023)
Article
Geosciences, Multidisciplinary
Seyed Ali Mazhari, Jalil Ghalamghash, Santosh Kumar, J. Gregory Shellnutt, Fernando Bea
JOURNAL OF ASIAN EARTH SCIENCES
(2020)