Article
Geosciences, Multidisciplinary
Irina. V. Karmysheva, Vladimir G. Vladimirov, Sergey N. Rudnev, Vladislav A. Yakovlev, Dina V. Semenova
Summary: Accretionary-collisional events at the western margin of the Tuva-Mongolian microcontinent explain the contradictory Cambrian geodynamic history of the western Central Asian Orogenic Belt. The Erzin metamorphic complex in the tectonic Erzin zone is composed of high-grade metamorphic rocks formed under variable metamorphic conditions. The complex underwent multiple stages of ductile deformation, marking a collisional event at 495 Ma.
JOURNAL OF ASIAN EARTH SCIENCES
(2021)
Article
Geochemistry & Geophysics
Durgalakshmi, K. Sajeev, Ian S. Williams, D. Harinadha Reddy, M. Satish-Kumar, Niels Joens, Sanjeewa P. K. Malaviarachchi, Vinod O. Samuel, P. M. George
Summary: The early Palaeozoic ultrahigh-temperature metamorphism in eastern Gondwana began with Gondwana amalgamation around 580 million years ago and lasted for at least 50 million years. Peak metamorphism occurred almost simultaneously in Antarctica, Sri Lanka, southern India, and Madagascar, with similar peak conditions at around 1020-1040 degrees Celsius and 0.8 GPa. The East African Orogeny before 600 million years ago preheated the crust of eastern Gondwana for about 60 million years, leading to the UHT conditions during the collision of East and West Gondwana.
JOURNAL OF PETROLOGY
(2021)
Article
Geochemistry & Geophysics
Haiqi Yuan, Jian Wang, Zhipeng Xie, Jianguo Liu, Jinlin Liu
Summary: The eclogites from the Guanshan and Yangkou areas of the Sulu orogen are composed of garnet, omphacite, phengite, amphibole, quartz/coesite, rutile, and ilmenite. The mineral assemblages and phase equilibria modeling indicate two stages of metamorphism: prograde associated with quick subduction and retrograde associated with quick exhumation. These stages are consistent with the regional metamorphic events with ages of 245, 227, and 195 Ma.
Article
Geochemistry & Geophysics
Ines Pereira, Craig D. Storey, James R. Darling, Hugo Moreira, Robin A. Strachan, Peter A. Cawood
Summary: Earth is unique within the Solar System with its active plate tectonic regime. The timing of the development of plate tectonics on Earth is still debated, with some evidence suggesting it could have been operational as early as the Archaean. By examining detrital rock records and using rutile as a proxy for tracking low T/P metamorphism, researchers have been able to trace the occurrence of different metamorphic conditions through geological time. The study confirms that low T/P metamorphism has been operating on Earth since at least the late Palaeoproterozoic.
EARTH AND PLANETARY SCIENCE LETTERS
(2021)
Article
Geology
Botao Li, Hans-Joachim Massonne, Xiaoping Yuan
Summary: Contrasting views exist regarding the evolution of metamorphic rocks in the southeastern Pohorje Mountains. This study examined a micaschist sample and found that it experienced ultrahigh-pressure metamorphism in the Late Cretaceous, followed by contact metamorphism induced by the intrusion of the Pohorje pluton. These findings contribute to a geodynamic model for the region, which involves subduction of oceanic and continental crusts and intracontinental subduction caused by transpression.
JOURNAL OF METAMORPHIC GEOLOGY
(2023)
Article
Geology
Haiqi Yuan, Jian Wang, Keiko Hattori, Yanchen Yang, Jinlin Liu, Zhipeng Xie
Summary: The translation mentions that the Yangkou area in the Sulu ultrahigh pressure metamorphic belt records three stages of metamorphism, which is of great importance for understanding the influence of plate tectonics on the continental crust.
INTERNATIONAL GEOLOGY REVIEW
(2023)
Article
Geology
Jean-Baptiste Jacob, Stephane Guillot, Daniela Rubatto, Emilie Janots, Jeremie Melleton, Michel Faure
Summary: The study confirms the age of Variscan high-pressure metamorphism in the Palaeozoic basement of the western Alps, with ages of 456 ± 4 Ma and 448 ± 6 Ma obtained from eclogites. The peak pressure stage in the retrogressed eclogites was estimated to be >1.4 GPa at 690-740 degrees C, followed by decompression. Metamorphic zircon rims yield U-Pb dates scattering between 340 and 310 Ma, representing late stages of melt crystallization. The development of a mylonitic S2 foliation correlates with retrogression in the amphibolite facies during the mid-late Carboniferous, indicating exhumation of eclogites mixed with mid-crustal felsic lithologies.
JOURNAL OF METAMORPHIC GEOLOGY
(2021)
Article
Geology
Rahmi Melih Cortuk, Omer Faruk Celik, Mutlu Ozkan, Andrea Marzoli, Anil Alkan
Summary: The metamorphic sole rocks found in the Pinarbasi Ophiolite in Turkey are well-preserved rock units that provide insights into intra-oceanic subduction and obduction events in the Tethys Ocean. These rocks consist of various types and display different geochemical signatures, indicating different metamorphic conditions and depths within the subduction zone.
INTERNATIONAL GEOLOGY REVIEW
(2023)
Article
Geochemistry & Geophysics
Karolina Kosminska, Jane A. Gilotti, William C. McClelland, Matthew A. Coble, Jay B. Thomas
Summary: Garnet-kyanite-staurolite assemblages with late amphibole porphyroblasts were found in garbenschists in northernmost Ellesmere Island, Canada. The Petersen Bay Assemblage, consisting of this garbenschist and carbonate olistoliths, displays parallel isograds that indicate an increase in metamorphic grade towards the Pearya contact. However, a Cenozoic strike-slip fault disrupts the earlier accretionary relationship. The late amphibole growth suggests disequilibrium conditions. Model comparisons and quartz inclusions in garnet provide insights into the P-T history.
JOURNAL OF PETROLOGY
(2022)
Article
Geochemistry & Geophysics
Haiqi Yuan, Jian Wang, Keiko Hattori
Summary: Three types of eclogites were identified in the Xiaoxinzhuang area in the northern Sulu ultrahigh pressure (UHP) terrene. They exhibit different mineral compositions, characteristics, and distribution patterns. The rocks underwent UHP metamorphism, revealing a unique pressure-temperature path compared to other areas in the Sulu UHP terrane.
Article
Geosciences, Multidisciplinary
Vincenzo Festa, Annamaria Fornelli, Francesca Micheletti, Richard Spiess, Fabrizio Tursi
Summary: In this study, the significance of mylonitic reworking in the Serre Massif of Calabria, Italy is revealed through a multidisciplinary approach. The study investigates the structural, microstructural, and petrologic changes in a shear zone affecting Variscan lower crustal rocks. The findings suggest that this shear zone is of prime importance and challenge the previous understanding of the region as an undisturbed continuous section of the Variscan crust. The role of (eo-)Alpine high-pressure tectonics in the Serre Massif is highlighted, indicating a complete rejuvenation of the Variscan basement.
Article
Geology
Yingde Jiang, Pavla Stipska, Karel Schulmann, Carmen Aguilar, Sheng Wang, Robert Anczkiewicz, Jian Zhang, Pengfei Li, Francis Chopin
Summary: The study of a representative region in the central part of the Chinese Altai reveals a complex relationship between Barrovian- and Buchan-type metamorphic series, indicating different evolutionary processes of metamorphism in the geological history.
JOURNAL OF METAMORPHIC GEOLOGY
(2022)
Article
Geochemistry & Geophysics
Sampriti Basak, Eric Hasenstab, Santanu Kumar Bhowmik, Axel Gerdes, Somnath Dasgupta, Carsten Muenker, Gr. Ravindra Kumar, Sumit Chakraborty
Summary: Studying high-grade metamorphic rocks in a crustal-scale shear zone can provide insights into the Archean tectonic processes. Petrological investigations reveal different compositions and reaction histories of these rocks. By using thermobarometry, phase equilibria modeling, and geochronology, a multi-stage P-T-t history was reconstructed, suggesting an early form of peel-back styled orogenesis and intracrustal differentiation.
JOURNAL OF PETROLOGY
(2023)
Article
Geology
D. Patias, L. F. Cury, F. M. Faleiros, M. Calderon, S. Siga Jr, T. Theye
Summary: The study reveals a clockwise Pressure-Temperature-time metamorphic evolution in the Paranagua Terrane and compares it with other tectonic belts, showing contrasting metamorphic evolutions between South America and Africa during West Gondwana assembly. The Paranagua Terrane experienced three tectonometamorphic stages, with the first two associated with collisional processes and the third with post-collisional processes. This dataset provides insights into the evolution of southwest Gondwana units.
INTERNATIONAL GEOLOGY REVIEW
(2021)
Article
Geosciences, Multidisciplinary
Lei Zou, Jing-Hui Guo, Chong-Hui Yang, Li-Lin Du, Ping-Hua Liu
Summary: The Zanhuang Complex in the North China Craton consists of Archean-Palaeoproterozoic rocks, with garnet-bearing pelitic gneisses showing three distinct mineral assemblages corresponding to three metamorphic stages. Petrological and geochronological evidence indicates a continuous continental collision and rapid tectonic uplift around 1839-1831 Ma, providing insights into the tectonic evolution of the Trans-North China Orogen.
JOURNAL OF ASIAN EARTH SCIENCES
(2021)
Article
Geosciences, Multidisciplinary
Gaetano Ortolano, Eugenio Fazio, Roberto Visalli, G. Ian Alsop, Mario Pagano, Rosolino Cirrincione
JOURNAL OF STRUCTURAL GEOLOGY
(2020)
Article
Geosciences, Multidisciplinary
G. Ortolano, R. Visalli, E. Fazio, P. Fiannacca, G. Godard, A. Pezzino, R. Punturo, V Sacco, R. Cirrincione
INTERNATIONAL JOURNAL OF EARTH SCIENCES
(2020)
Article
Computer Science, Information Systems
Gaetano Ortolano, Alberto D'Agostino, Mario Pagano, Roberto Visalli, Michele Zucali, Eugenio Fazio, Ian Alsop, Rosolino Cirrincione
Summary: ArcStereoNet is a new stereographic projection toolbox based on ArcGIS(R) and implemented using Python 2.7. It allows for flexible application of statistical methods, provides high-quality graphic outputs, and has an intuitive GUI interface.
ISPRS INTERNATIONAL JOURNAL OF GEO-INFORMATION
(2021)
Article
Computer Science, Information Systems
Roberto Visalli, Gaetano Ortolano, Gaston Godard, Rosolino Cirrincione
Summary: The new Micro-Fabric Analyzer (MFA) utilizes X-ray and optical image features for quantitative extrapolation of rock microstructural features, allowing for more comprehensive analysis compared to traditional edge mineral grain detectors. The MFA toolbox enables low-cost and user-friendly quantification of mineral types, integrated with micro-X-ray maps for extrapolating elemental distribution maps.
ISPRS INTERNATIONAL JOURNAL OF GEO-INFORMATION
(2021)
Article
Geosciences, Multidisciplinary
Manuel Roda, Michele Zucali, Luca Corti, Roberto Visalli, Gaetano Ortolano, Maria Iole Spalla
Summary: The Rocca Canavese Thrust Sheets Unit (RCTU) is a subduction-related melange situated between Alpine subduction complex and Southalpine domain. It is characterized by mylonitic to ultra-mylonitic zone in the tectonic contact area, with pre-mylonitic parageneses preserved in some rocks. The coupling of RCTU, EMC, and LM occurred during the Alpine evolution, showing three deformation and metamorphic stages.
SWISS JOURNAL OF GEOSCIENCES
(2021)
Article
Geochemistry & Geophysics
Jean-Francois Moyen, Vojtech Janousek, Oscar Laurent, Olivier Bachmann, Jean-Baptiste Jacob, Federico Farina, Patrizia Fiannacca, Arnaud Villaros
Summary: This paper discusses the two competing paradigms regarding the formation of granitic magmas and their implications, emphasizing that both views are based on a large body of evidence and propose that each of them is relevant to some portions of the Earth.
Article
Geochemistry & Geophysics
Michele Zucali, Luca Corti, Manuel Roda, Gaetano Ortolano, Roberto Visalli, Davide Zanoni
Summary: By utilizing the Quantitative X-ray Maps Analyzer (Q-XRMA), this study investigated three samples of meta-acidic rocks with pre-Alpine metamorphic relicts from the Sesia-Lanzo Zone, aiming to analyze reacting zones between pre-Alpine and Alpine mineral phases. The quantitative data treatment of X-ray images allowed for the isolation and quantitative investigation of local paragenetic equilibria, providing insights into the pre-Alpine metamorphic scenario and the influence of pre-Alpine metamorphic inheritance on Alpine tectonic evolution.
Article
Geosciences, Multidisciplinary
Rosanna Maniscalco, Eugenio Fazio, Rosalda Punturo, Rosolino Cirrincione, Agata Di Stefano, Salvatore Distefano, Martina Forzese, Gabriele Lanzafame, Giusy Simona Leonardi, Sergio Montalbano, Alessandra Giovanna Pellegrino, Antonino Raele, Giuseppe Palmeri
Summary: In this study, a multi-scale and multidisciplinary approach was used to investigate the role of tectonic and diagenetic structures in enhancing or reducing the porosity of carbonate rocks. The results show that fractures and faults have minimal impact on porosity, while stylolites exhibit certain porosity.
Article
Geosciences, Multidisciplinary
Patrizia Fiannacca, Damiano Russo, Eugenio Fazio, Rosolino Cirrincione, Manish A. Mamtani
Summary: The Serre Batholith in Central Calabria represents the intermediate portion of late Variscan continental crust, with upper levels composed of two-mica granodiorites and granites, and lower levels of weakly peraluminous granodiorites. The granitoid rocks in the batholith exhibit deformation microstructures due to tectonic stresses, with a magnetic foliation showing a shortening axis oriented NW-SE. Ongoing studies aim to further investigate the relationship between regional tectonic structures and the emplacement of the late-Variscan Serre Batholith granitoids.
Article
Geochemistry & Geophysics
R. Lombardo, P. Fiannacca, R. Cirrincione
Article
Geochemistry & Geophysics
Huichuan Liu, Alan R. Hastie, Chiara Maria Petrone
Summary: This study conducted isotope analyses on two ocean island basalt (OIB)-associated enriched mafic intrusions in the Yunnan-Burma region, and found that these rocks may have originated from the subduction recycling of marine sediments and altered oceanic crust.
Article
Geochemistry & Geophysics
L. Notini, M. Scambelluri, A. Tommasi, A. Zanetti, F. Ferri, A. Rodriguez-Vargas, E. Rampone
Summary: This study provides important petrologic information on the mantle wedge above an active subduction zone in Southern Colombia. The researchers analyzed a unique suite of rock samples and found evidence of hydration, metasomatism, and partial melting in the mantle wedge. They also observed variations in lithotypes, textures, and mineral abundance, indicating different interactions with melts and fluids. This study sheds light on the complex petrological processes occurring in the mantle wedge and contributes to our understanding of subduction zone dynamics.
Article
Geochemistry & Geophysics
Sourav Bhattacharjee, Aniket Chakrabarty, Roger H. Mitchell, Suresh Chandra Patel, Evgeniy N. Kozlov, Ekaterina N. Fomina, Monojit Dey, Supratim Pal
Summary: The Hogenakkal complex in India consists of silicate-rich and silicate-poor carbonatites and clinopyroxenites. The formation of carbonatite is influenced by silicate minerals. The carbohydrothermal mineralization in the carbonatites is induced by magma-derived fluids and interactions with the surrounding rocks.
Article
Geochemistry & Geophysics
Jia-Min Wang, Kyle Patrick Larson, Jin-Jiang Zhang, Liang Zhao, Fu-Yuan Wu
Summary: The role of collisional belts in the global carbon budget is controversial. This study reveals a previously unrecognized carbon source in the collisional orogen of the Himalayas, where metamorphism of carbonate-bearing rocks in the hanging wall resulted in significant CO2 degassing.
Article
Geochemistry & Geophysics
Joseph Martial Akame, Elson Paiva Oliveira, Vinciane Debaille, Marc Poujol, Bernhard Schulz, Dieudonnee Bisso, Fabien Humbert, Serge Parfait Koah Na Lebogo, Philmont Zo'o Zame
Summary: Archean granitoids play key roles in the crustal evolution and can provide important insights into early geologic processes.
Article
Geochemistry & Geophysics
Xiguang Huang, Jun He, Jingxin Zhao, Jingzhao Dou, Weiyong Li, Aimin Hu, Ge Liu, Yiru Ji, Fukun Chen, Shuangqing Li
Summary: This study investigates the zircon ages and whole-rock geochemical data of Late Paleozoic magmatic rocks in the Western Yunnan Tethyan belt to identify the origin and mechanism of mantle melting. The results suggest that these magmatic rocks may originate from different mantle domains that were metasomatized by slab-derived fluids and sediment-derived melts.