Article
Geology
Shashi Tamang, Chiara Groppo, Frederic Girault, Franco Rolfo
Summary: Recent studies have shown that kinetic factors can affect the nucleation of garnet, causing a delay in its appearance compared to equilibrium predictions. This study focuses on the garnet nucleation and growth in aluminous metapelites from the Barrovian inverted metamorphic pile in central Nepal. The results suggest that the bulk-rock composition may influence the degree of garnet nucleation overstepping, and the implications of this overstepping on the P-T evolution of the metamorphic sequence were explored.
JOURNAL OF METAMORPHIC GEOLOGY
(2023)
Article
Geology
Qiang-Qiang Zhang, Xiao-Ying Gao, Yong-Fei Zheng
Summary: The study utilized a composite approach to determine a reliable P-T path for eclogite from the Tongbai orogen, linking zircon U-Pb ages to specific P-T intervals. The analysis revealed that the eclogite experienced multistage metamorphic evolution, characterized by compressional heating and two stages of isothermal decompression. Metamorphic zircon domains in eclogite showed distinct characteristics in different stages of metamorphism.
JOURNAL OF METAMORPHIC GEOLOGY
(2021)
Article
Geochemistry & Geophysics
Tamas Spranitz, Csaba Szabo, Mattia Gilio, Matteo Alvaro, Michaela Blazekova, Patrik Konecny, Tamas Vaczi, Marta Berkesi
Summary: Fluid and mineral inclusions in metamorphic rocks play a crucial role in understanding fluid-involved processes in subduction zones. This study focuses on ultramafic granulite from the Cabo Ortegal Complex in Spain, using quartz-in-garnet and zircon-in-garnet Raman spectroscopy to determine the entrapment conditions of mineral and fluid inclusions. The findings confirm the reliability of elastic thermobarometry on mineral inclusions in determining the entrapment P-T conditions. Rating: 8 out of 10.
Article
Geology
Shah Wali Faryad, Josef Jezek, Jan Kulhanek
Summary: This study presents the petrological observations and diffusion modelling results of garnet from high-pressure to ultrahigh-pressure metamorphic rocks in the Western Gneiss Region. The results reveal the evolution of Pre-Caledonian granulite facies and Caledonian eclogite facies metamorphic events in these rocks, with preservation of compositional gradients and relaxation processes. Calculations indicate a pressure of up to 2.6 GPa and a temperature of 650 degrees C during the eclogite facies event. The study also provides insights into the cooling rate and exhumation rate of the rocks during their geological history.
JOURNAL OF METAMORPHIC GEOLOGY
(2022)
Article
Geochemistry & Geophysics
Byeong Jun Park, Hyeong Soo Kim
Summary: Garnet amphibolites with relics of mafic granulite have been discovered in the Odaesan Complex and Taebaeksan Basin on the Korean Peninsula. Through mineral equilibrium modeling, the conditions, processes, and products of garnet metamorphism and metasomatism were revealed. This study is of great significance for understanding the geological evolution of the eastern margin of the Korean Peninsula.
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
(2022)
Article
Geochemistry & Geophysics
Hao Wang, Wenjiao Xiao, Brian F. Windley, Qian W. L. Zhang, Zhou Tan, Chunming Wu, Mengyan Shi
Summary: Subduction zones play a crucial role in reconstructing tectonic configurations and convergent geodynamics. In this study, new petrologic and geochronologic data were used to reveal the complex metamorphic structure and history of the subduction-exhumation channel in the Dunhuang area of China. The findings provide important insights into the reconstructions of proto-Asia and subduction dynamics.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2022)
Article
Geochemistry & Geophysics
Mei Xia, Qiang-Qiang Zhang, Xiao-Ying Gao
Summary: The metamorphic evolution paths of low-temperature ultrahigh-pressure eclogites can reliably record the thermal structure of subduction zones. The study carried out in the Dabie orogen suggests that the thermal structure of the continental subduction zone shows a gradually decreasing thermal gradient with depth.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2023)
Article
Geology
Pauline Jeanneret, Iwona Klonowska, Christopher Barnes, Jaroslaw Majka, Johanna Holmberg, Mattia Gillio, William Nachlas, Matteo Alvaro, Karolina Kosminska, Henning Lorenz, Thomas Zack, Anna Ladenberger, Hemin Koyi
Summary: The tectonometamorphic evolution of the Lower Seve Nappe in the Scandinavian Caledonides was characterized using various P-T estimation techniques. The results show that quartz inclusions in garnet provide critical data to constrain the evolutionary path of the metasedimentary rocks.
JOURNAL OF METAMORPHIC GEOLOGY
(2023)
Article
Geochemistry & Geophysics
Chenying Yu, Ting Yang, Jian Zhang, Guochun Zhao, Peter A. Cawood, Changqing Yin, Jiahui Qian, Peng Gao, Chen Zhao
Summary: The Eastern Block of the North China Craton exhibits a greenstone-granite rock association with dome-and-keel structures. Through numerical models, researchers identified different P-T-t paths resulting from crustal-scale sagduction and proposed that these geological features were likely developed under a mantle plume related crustal-scale sagduction geodynamic regime.
EARTH AND PLANETARY SCIENCE LETTERS
(2022)
Article
Environmental Sciences
Liang Yuan, Weisheng Lu, Fan Xue
Summary: By combining big data analytics and traditional probability theories, this research developed a BD-P model for estimating the composition of construction waste, achieving an accuracy of 90.2% and a speed of around 52 seconds per estimation. The study successfully addressed the challenge faced by waste management facility operators in estimating construction waste composition.
JOURNAL OF ENVIRONMENTAL MANAGEMENT
(2021)
Article
Geochemistry & Geophysics
G. Cruciani, M. Franceschelli, R. Carosi, C. Montomoli
Summary: This study investigates micaschists in the southeastern sector of the Posada-Asinara Shear Zone in the Axial Zone of the Sardinia Variscan chain to reconstruct their metamorphic evolution and P-T history. The micaschists experienced polyphase ductile deformation and are characterized by abundant garnet crystals with strong compositional zoning. The P-T path of the micaschists is determined to be clockwise and consists of two separate stages.
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
Geochemistry & Geophysics
Shujuan Jiao, Noreen J. Evans, Jinghui Guo, Ian C. W. Fitzsimons, Jian-Wei Zi, Bradley J. McDonald
Summary: The identification of peritectic and retrograde garnets based on chemical signatures provides insights into the P-T evolution of UHT granulites, showing an earlier high-pressure peritectic garnet formation during prograde partial melting and a late abundant retrograde formation during post-peak cooling stage. The change in elements such as Zr, Ti, Ca, Y, and Eu/Eu* can distinguish different garnet formation events and contribute to our understanding of the cause of UHT metamorphism and geodynamic evolution.
AMERICAN MINERALOGIST
(2021)
Article
Geosciences, Multidisciplinary
Renata da Silva Schmitt, Renato Moraes, Rodrigo Vinagre, Thayla Almeida Teixeira Vieira, Julio Cezar Mendes, George Luiz Luvizotto, Raphaela Lopes de Andrade Silva, Silvia Regina de Medeiros
Summary: This paper presents petrochronological data on the structural and stratigraphic relations of Ediacaran basement and cover gneisses during the Ediacaran-Cambrian Btizios orogeny in southeastern Brazil. The data reveals distinct crustal levels and contrasting P-T-t paths during convergent tectonics. The findings suggest the existence of a low-angle subduction zone and present the highest recorded pressure in Ediacaran-Cambrian metamorphic rocks.
PRECAMBRIAN RESEARCH
(2022)
Article
Geosciences, Multidisciplinary
Rafael G. Motta, Ian C. W. Fitzsimons, Renato Moraes, Tim E. Johnson, Sheila Schuindt, Beatriz Y. Benetti
Summary: Through various methods, this study constrained the pressure-temperature-time history of granulites from the Socorro-Guaxupe Nappe in Southern Brasilia Orogen, revealing a protracted regional metamorphic event lasting over 30 million years during the collision and assembly of West Gondwana.
PRECAMBRIAN RESEARCH
(2021)
Article
Geochemistry & Geophysics
Zhen-Min Ge, Xiao-Long Huang, Wei Xie, Tobias W. Hofig, Fan Yang, Yang Yu, S. Khogenkumar Singh
Summary: The mantle source composition of the nascent oceanic crust in the central part of the Gulf of California has been investigated using basaltic glass samples. These samples show trace element patterns similar to enriched mid-ocean ridge basalts, suggesting that the nascent oceanic crust in the Guaymas Basin might be generated through partial melting of a depleted mantle source metasomatized by subducted slab materials.
Article
Geochemistry & Geophysics
Jean-Michel Brazier, Katja E. Goetschl, Martin Dietzel, Vasileios Mavromatis
Summary: This study estimated the distribution coefficient of Zn2+ between calcite/aragonite and reactive fluids and found that the growth rate strongly influences D-Zn(2+) in both minerals. Additionally, a linear correlation was found between D-Zn(2+) and the saturation degree of the reactive fluid.
Article
Geochemistry & Geophysics
Ming Lei, Michele Lustrino, Jifeng Xu, Zhiqiang Kang, Zhengfu Guo, Jianlin Chen
Summary: This study presents a comprehensive geochronological, mineralogical, and geochemical analysis of olivine leucitites in the Maiga area of southern Tibet, suggesting that these rocks originate from a carbonated peridotite mantle source and highlighting the possibility of carbonates being recycled deep into the mantle during continental subduction.
Article
Geochemistry & Geophysics
Yuntao Ye, Xiaomei Wang, Huajian Wang, Haifeng Fan, Zhigang Chen, Qingjun Guo, Ziteng Wang, Chaodong Wu, Donald E. Canfield, Shuichang Zhang
Summary: Phosphorus is an essential element for life and its cycle in the ocean is closely connected with the carbon and oxygen cycles. The study of phosphate oxygen isotopes can provide insights into various reactions related to phosphorus. By analyzing carbonate fluorapatite samples from the Mesoproterozoic Era in North China, it was found that the oxygen isotope values were lower compared to modern samples, indicating a warmer climate during that time period and a potential reason for the scarcity of phosphorite.
Article
Geochemistry & Geophysics
Vincent Busigny, Oanez Lebeau, Didier Jezeduel, Carine Chaduteau, Sean Crowe, Magali Ader
Summary: This study conducted high-precision Mo isotope research on hydrothermal metal sulfides from a porphyry copper deposit in Southwest China and found that different stages of mineralization have distinct Mo isotope compositions, providing valuable insights into the behavior of Mo isotopes in magmatic-hydrothermal systems.
Article
Geochemistry & Geophysics
Min Ji, Xiao-Ying Gao, Yong-Fei Zheng, Bing Gong
Summary: The study examines the anatectic mechanisms in the Himalayan orogen, finding that pressure and temperature control the reaction, while water content mainly affects the solid-phase composition. Dehydration and hydration melting likely occur at different depths in the crust. This research provides important insights into the melting processes in collisional orogens.