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10 results for “metasomatism”

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zenodo36/100

Metasomatic reactions between Archean dunite and trondhjemite at the Seqi Olivine Mine in Greenland

<p>Supplementary materials relating to the paper: Metasomatic reactions between Archean dunite and trondhjemite at the Seqi Olivine Mine in Greenland by Wyatt et al.</p>

opencc-by-4.0Nov 2019View details →
zenodo36/100

Additional data and models for the article "Role of metasomatism in the development of the East African Rift at the Northern Tanzanian Divergence: Insights from 3D magnetotelluric modelling."

<p>Additional data and models for the article "Role of metasomatism in the development of the East African Rift at the Northern Tanzanian Divergence: Insights from 3D magnetotelluric modelling."</p> <p>This data package includes:</p> <p>1-ModEM rho and dat format files of the final preferred model.</p> <p>2-vtk version of this model</p> <p>3-Scripts to plot the MT models</p> <p>4-Water content models calculated with MATE</p> <p>5-Scripts to plot the water content models</p> <p>6-Parameter files used in water calculation with MATE</p> <p>7- EDI files used in the model.</p>

opencc-by-4.0Aug 2023View details →
zenodo36/100

Barium isotope variation during fluid-rock interaction at forearc depths: evidence from the high-pressure fluid-metasomatized rocks in the Eastern Alps

<p><a name="OLE_LINK7"></a><a name="OLE_LINK1"></a><span><span>The supporting information presents the analytical methods of whole-rock major-trace element compositions and Mg&ndash;Fe isotope compositions , as well as whole-rock major-trace elements and Fe&ndash;Mg&ndash;Sr isotope data</span></span><span><span>.</span></span></p>

opencc-by-4.0Dec 2023View details →
zenodo36/100

Carbonatite metasomatism in subvolcanic settings: implications for magmatic evolution and eruptive style

<p>The supplementary tables S1-S4 which support for the manuscript &quot;Carbonatite metasomatism in subvolcanic settings: implications for magmatic evolution and eruptive style&quot;</p>

opencc-by-4.0Oct 2023View details →
zenodo36/100

Strong Physical Contrasts across Two Mid-lithosphere Discontinuities beneath the Northwestern United States: Evidence for Cratonic Mantle Metasomatism

<p>Data files for "Strong Physical Contrasts across Two Mid-lithosphere Discontinuities beneath the Northwestern United States: Evidence for Cratonic Mantle Metasomatism". See ReadMe.txt for details.</p>

opencc-by-4.0Oct 2023View details →
zenodo32/100

Fore-arc metasomatism by hybrid slab fluids during subduction initiation: Sr–Mg–Ca isotopes of rodingite, western Yarlung Zangbo suture zone

<p>&nbsp; &nbsp; Subduction zone metasomatism is critical for Earth&rsquo;s material exchanges, yet understanding slab dehydration, particularly deserpentinization beneath fore-arcs, remains challenging. Here, we present Sr&ndash;Mg&ndash;Ca isotopic data for the Purang rodingites in the western Yarlung-Zangbo suture zone (YZSZ). These rodingites, dominated by amphibolite- to greenschist-facies minerals like tremolite, magnesiohornblende, and chlorite, exhibit cumulate textures and rare earth element patterns resembling troctolites or gabbronorites, presumably formed beneath a seafloor spreading center. The rodingites are enriched in large ion lithophile elements and depleted in high field strength elements. They show higher initial <sup>87</sup>Sr/<sup>86</sup>Sr ratios (0.7067&ndash;0.7075) and elevated&nbsp; &delta;<sup>26</sup>Mg values (&ndash;0.22 &plusmn; 0.07&permil; to &ndash;0.13 &plusmn; 0.02&permil;) compared to pristine oceanic basalts, while their &delta;<sup>44/40</sup>Ca values (0.72 &plusmn; 0.02&permil; to 0.87 &plusmn; 0.03&permil;) correspond to mid-ocean ridge basalts (MORB). These features imply fore-arc mantle metasomatism of an original MOR-derived protolith at &lt;40 km slab depth, driven by Sr- and Mg-rich fluids from clay-rich sediments and serpentinitized mantle, respectively. The measured Sr and Mg isotope compositions can be reproduced by mixing a MORB-like protolith with hybrid fluids derived from 70&ndash;30% clays and 30&ndash;70% serpentinites, with a fluid-to-rock ratio of approximately 1:3&ndash;1:5. Combined with studies on YZSZ metamorphic soles, we propose this metasomatism occurred during incipient subduction of the Neo-Tethys oceanic rocks. Our studies highlight the significance of deserpentinization at shallow fore-arc mantle settings during subduction initiation and suggest that subducting slabs exhibit more varied dehydration characteristics than previously recognized.</p>

opencc-by-4.0Jun 2024View details →
zenodo32/100

Mantle xenoliths used in "High P-T sound velocities of amphiboles: Implications for low-velocity anomalies in metasomatized upper mantle"

<p>Mineral proportions in hydrous-mineral-bearing mantle xenoliths collected worldwide and their calculated sound velocities in this study. &nbsp;</p>

opencc-by-4.0May 2023View details →
zenodo32/100

Data for Lindquist et al., Metasomatism and slow slip: talc production along the flat subduction plate interface beneath Mexico (Guerrero)

<p>A compilation of data supporting our 2023 G-Cubed manuscript submission &quot;Metasomatism and slow slip: talc production along the flat subduction plate interface beneath Mexico (Guerrero),&quot; including<br> (1) and Excel file containing bulk compositions and phase solution models used in our Perple_X modeling</p> <p>(2) text files of all the output Perple_X data that were used for calculations of results presented in the manuscript, including mineral modes, densities, and silica contents</p>

opencc-by-4.0Jun 2023View details →
zenodo32/100

Mapping the Structure and Metasomatic Enrichment of the Lithospheric Mantle Beneath the Kimberley Craton, Western Australia

<p>SUPPLEMENT&nbsp;FILE&nbsp;1: LA-ICP-MS and EPMA analyses for pyrope garnet and Cr diopside used in study.&nbsp;</p>

opencc-by-4.0Aug 2023View details →
zenodo28/100

Ba-Mg isotopes in high Ba-Sr granites record melt-metasomatized mantle and crustal growth

Open the record for dataset details and reuse information.

opencc-by-4.0May 2024View details →

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