Article
Geochemistry & Geophysics
Qi-Qi Pan, Yan Xiao, Ben-Xun Su, Xia Liu, Meng-Meng Cui, Jing Wang, Ibrahim Uysal
Summary: This study presents observations and analyses of mantle harzburgites in the Lycian ophiolite of SW Turkey, revealing their formation in a suprasubduction zone mantle wedge with well-preserved metasomatic signatures.
Article
Geochemistry & Geophysics
Nicholas Arndt, Carole Cordier, Anne-Marie Boullier, Valentina Batanova, Valerie Magnin, Nathaniel Findling
Summary: Kimberlites contain olivine nodules with a wide range of Fo content. These nodules, regardless of their Fo content, have similar sizes, internal textures, and habits. They are believed to have a common origin with olivines in the megacryst suite, formed through interactions between mantle peridotite and CO2-rich fluid. This interaction occurred near the base of the lithosphere, not during kimberlite ascent.
JOURNAL OF PETROLOGY
(2022)
Article
Geochemistry & Geophysics
Xiang Zhou, Jianping Zheng, Yibing Li, Hui Zhu, William L. Griffin, Suzanne Y. O'Reilly
Summary: The Harzburgite-dunite associations in the Yushigou ophiolitic complex provide insights into melt migration and melt-rock interaction above a subduction zone. A three-stage model has been proposed to describe the history of melt channel formation in the oceanic arc mantle, revealing the complex processes involved in the interaction between multiple batches of melt or fluid and a lithospheric mantle wedge dunitic channel system.
JOURNAL OF PETROLOGY
(2021)
Article
Geochemistry & Geophysics
M. Jerram, P. Bonnand, J. Harvey, D. Ionov, A. N. Halliday
Summary: Chromium isotope compositions of mantle-derived xenoliths have been determined, showing a range of -0.33% to 0.43%. The process of partial melting is proposed to alter the chromium isotope composition of the mantle residue, possibly related to interactions with low degree partial melts.
GEOCHIMICA ET COSMOCHIMICA ACTA
(2022)
Article
Geochemistry & Geophysics
Yue Cai, Alexandra Yang Yang, Steven L. Goldstein, Charles H. Langmuir, Peter J. Michael, James R. Cochran, Wenfang Zhang, Di Wang, Louise Bolge
Summary: Through a high-resolution geochemical study of the EVZ2 section of the Arctic Gakkel Ridge, a group of Isotopically Enriched, Incompatible Element Depleted MORB (IED-MORB) was identified. These IED-MORB are believed to be products of two stages of mantle melting and may erupt through pre-existing crustal weaknesses with enriched isotopic compositions.
Article
Geochemistry & Geophysics
Merislava Anguelova, Manuela A. Fehr, Eiichi Takazawa, Maria Schoenbaechler
Summary: Titanium isotopes are a promising tracer for magmatic processes, and there are variations in titanium isotopes in mantle rocks. High heavy titanium isotopes might originate from metasomatism in the mantle wedge.
GEOCHIMICA ET COSMOCHIMICA ACTA
(2022)
Article
Geochemistry & Geophysics
David Jousselin, Adolphe Nicolas, Francoise Boudier, Laurie Reisberg, Mathilde Henri, Marie Nicolle
Summary: Our understanding of melt distribution in the lower crust and upper mantle at oceanic fast spreading centers is limited. Ophiolites on land can complement marine geological and geophysical observations. Magma accumulation and variations in melt layer thickness at the Moho transition zone provide insights into processes at oceanic ridges.
Article
Geosciences, Multidisciplinary
Anton Shatskiy, Altyna Bekhtenova, Ivan Podborodnikov, Anton Arefiev, Yulia G. Vinogradova, Konstantin D. Litasov
Summary: The study examined the interaction of natural eclogite with synthetic hydrous carbonate melts under varying conditions, revealing different mineral evolution outcomes, and indicating that hydrous K-and Na-K-carbonatite melts can coexist with eclogite at depths in the mantle, leading to different mineral assemblages.
Article
Geosciences, Multidisciplinary
Ben-Xun Su, Qi-Qi Pan, Yan Xiao, Jie-Jun Jing, Paul T. Robinson, Ibrahim Uysal, Xia Liu, Jian-Guo Liu
Summary: The traditional interpretation of mantle peridotites in ophiolites needs to be reconsidered as recent petrological and geochemical data suggest significant compositional variations and modifications in these rocks. The presence of interstitial spinel grains and widespread clinopyroxene suggests post-crystallization modifications. Amphibole and enriched Mg and Ca melts/fluids serve as evidence of the past presence of hydrous melts and indicate interactions between different lithologies. The mantle peridotites of ophiolites cannot be considered as paleo-oceanic lithospheric mantle and cannot be used for reconstructing ancient oceans or constraining global tectonic processes.
EARTH-SCIENCE REVIEWS
(2023)
Article
Geochemistry & Geophysics
Anton Shatskiy, Altyna Bekhtenova, Ivan Podborodnikov, Anton V. Areflev, Konstantin D. Litasov
Summary: The study reveals that potassium-rich carbonatite melts can maintain thermodynamic equilibrium with different types of olivine at high pressure and high temperature. Melts with Ca# < 30 result in wehrlitization, melts with Ca# ranging from 30 to 34 cause harzburgitization, and melts with Ca# > 34 induce wehrlitization. At a depth of about 200 km in the subcontinental lithospheric mantle, high-Mg sodium-rich dolomitic carbonatite melts are the only carbonate melts that can thermodynamically stable with garnet lherzolites.
EARTH AND PLANETARY SCIENCE LETTERS
(2022)
Article
Geochemistry & Geophysics
Delphine Klaessens, Laurie Reisberg, David Jousselin
Summary: This study investigates the formation and evolution mechanism of dunites in the peridotites from the Batin region of the Oman ophiolite. Structural and geochemical analysis reveals that dunites in the Batin region are structurally and chemically distinct from those in other regions, possibly due to the influence of large pulses of radiogenic melts during their formation. The study suggests that understanding the flow dynamics of melts through peridotites is crucial in explaining the formation of dunites in ophiolites.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Geochemistry & Geophysics
Oded Elazar, Ronit Kessel, Jin-Xiang Huang, Katharina Marquardt, Oded Navon
Summary: The study identified fluid/melt microinclusions in dusty garnets from the Roberts Victor mine in South Africa, which contain water, CO2, carbonate, and other elements that are enriched relative to the host garnet. The composition of the microinclusions resembles high-density fluids trapped in diamonds, suggesting a role of diamond forming fluids in mantle metasomatism.
Article
Geosciences, Multidisciplinary
Max Collinet, Ana-Catalina Plesa, Thomas Ruedas, Sabrina Schwinger, Doris Breuer
Summary: The composition of basaltic melts in equilibrium with the mantle on Mars can be determined through analysis of Martian meteorites and rover investigations. By using the MAGMARS melting model, researchers are able to replicate these primary melts and estimate the composition and temperature of the mantle regions they originated from. The findings suggest that most mantle sources are lacking in CaO and Al2O3, possibly indicating that they are either residue from melting or cumulates from an ancient magma ocean. The concentrations of Na2O, K2O, P2O5, and TiO2 vary and are often less depleted, suggesting that the sources may have been re-fertilized by fluids and low-degree melts or captured residual melts during the crystallization of the magma ocean. The mantle potential temperatures of these sources fall in the range of 1400-1500 degrees C, regardless of the time of melting, consistent with recent predictions from thermochemical evolution models.
GEOPHYSICAL RESEARCH LETTERS
(2023)
Article
Geochemistry & Geophysics
Chunguang Wang, Yan Liang, Wenliang Xu
Summary: Amphibole-bearing rock sequences are formed through crystallization of partially reacted melts during cooling in experiments where basaltic andesite and basalt with 4 wt% water are juxtaposed against lherzolite at high temperature and pressure conditions.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Geochemistry & Geophysics
Alexander A. Iveson, Madeleine C. S. Humphreys, Ivan P. Savov, Jan C. M. de Hoog, Stephen J. Turner, Tatiana G. Churikova, Colin G. Macpherson, Tamsin A. Mather, Boris N. Gordeychik, Lubomira Tomanikova, Samuele Agostini, Keiji Hammond, David M. Pyle, George F. Cooper
Summary: The chemistry of primitive arc rocks provides insights into the compositional variability in the mantle wedge and slab-derived inputs to subduction-related magmatism. By analyzing olivine-hosted melt inclusions from the Kamchatka arc, systematic variations in element ratios are observed, which provide evidence for subduction-related metasomatism and mantle melting degrees. Across-arc variations in B isotopes reflect variable contributions of slab-derived components to depleted mantle compositions, with signals of compositional heterogeneity preserved during magma assembly and storage in the crust.
EARTH AND PLANETARY SCIENCE LETTERS
(2021)
Article
Geochemistry & Geophysics
Yan Liang, Boda Liu
EARTH AND PLANETARY SCIENCE LETTERS
(2018)
Article
Geochemistry & Geophysics
Haoyuan Li, Nan Zhang, Yan Liang, Bingcheng Wu, Nicholas J. Dygert, Jinshui Huang, E. M. Parmentier
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
(2019)
Article
Geochemistry & Geophysics
Alexandra Yang Yang, Chunguang Wang, Yan Liang, C. Johan Lissenberg
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2019)
Article
Geochemistry & Geophysics
Chunguang Wang, Mauro Lo Cascio, Yan Liang, Wenliang Xu
GEOCHIMICA ET COSMOCHIMICA ACTA
(2020)
Article
Geochemistry & Geophysics
Veronique Le Roux, Yan Liang
Article
Geochemistry & Geophysics
Boda Liu, Yan Liang
EARTH AND PLANETARY SCIENCE LETTERS
(2019)
Article
Geochemistry & Geophysics
Boda Liu, Yan Liang
GEOCHIMICA ET COSMOCHIMICA ACTA
(2020)
Article
Geochemistry & Geophysics
Yan Liang
EARTH AND PLANETARY SCIENCE LETTERS
(2020)
Article
Geochemistry & Geophysics
Leif Tokle, Greg Hirth, Yan Liang, Paul Raterron, Nick Dygert
Summary: The viscosity of ilmenite is influenced by pressure and Mg-content, with ilmenite40 showing larger stress exponent and activation volume than ilmenite100. Ilmenite100 has significantly lower viscosity compared to dry olivine under conditions representative of the early ilmenite-bearing cumulate. Lunar mantle overturn may be dominated by longer wavelength downwellings in a dry lunar mantle, and by shorter wavelength downwellings in a wet lunar mantle during initial overturn.
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
(2021)
Article
Geochemistry & Geophysics
Chunguang Wang, Yan Liang, Wenliang Xu
Summary: Amphibole-bearing rock sequences are formed through crystallization of partially reacted melts during cooling in experiments where basaltic andesite and basalt with 4 wt% water are juxtaposed against lherzolite at high temperature and pressure conditions.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Geochemistry & Geophysics
Yan Liang, Zejia Ji, Boda Liu
Summary: This study investigated the REE abundance in clinopyroxene and orthopyroxene in residual spinel peridotites to understand mantle processes. It concluded that deducing melting parameters from bulk peridotite samples is more reliable than from clinopyroxene alone, and highlighted the different susceptibility of HREE in clinopyroxene and LREE in orthopyroxene to subsolidus redistribution.
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
(2021)
Article
Geochemistry & Geophysics
D. J. Cherniak, Y. Liang
Summary: This study characterizes the chemical diffusion of Ca in natural enstatite and explores its sensitivity to crystallographic orientation, oxygen fugacity, silica activity, and Ca concentration. The results show that Ca diffusion in enstatite is relatively insensitive to these factors, and the diffusion is slower than that of some other cations but faster than others. The obtained diffusion parameters are used to develop a model for the Ca-inopx thermometer and estimate the cooling rates of peridotites and pyroxenites.
GEOCHIMICA ET COSMOCHIMICA ACTA
(2022)
Article
Geochemistry & Geophysics
Yan Liang
Summary: Mixing in basalts is widely used to explain variations in radiogenic isotope ratios and highly incompatible trace elements. This study presents a new mixing model that considers the size, spatial location, and melting history of enriched and depleted mantle parcels. The results show that the compositions of pooled melt do not follow a single mixing curve, but instead define a mixing loop. Understanding these mixing processes is important for studying the chemical variations in mantle-derived melts.
JOURNAL OF PETROLOGY
(2022)
Article
Geochemistry & Geophysics
Kei Shimizu, Yan Liang, Chenguang Sun, Colin R. M. Jackson, Alberto E. Saal
AMERICAN MINERALOGIST
(2017)
Article
Geochemistry & Geophysics
Nick Dygert, Peter B. Kelemen, Yan Liang
EARTH AND PLANETARY SCIENCE LETTERS
(2017)