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4 results for “Ultra-depleted”

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zenodo36/100

Discovery of Ultra-depleted Melt Inclusion in Late Cretaceous Intraplate Basaltic Andesites in South China

<p>1. Supporting Information, including supplemental methods and figures.</p> <p>2. Datasets:</p> <p>Dataset S1. Compiled data including basaltic rocks from South China, MORBs, and Hawaii OIBs.</p> <p>Dataset S2. Whole-rock major oxide, trace element, and Sr-Nd-Pb-Hf isotopic compositions.</p> <p>Dataset S3. Olivine chemical compositions.</p> <p>Dataset S4. Measured and corrected major element compositions of melt inclusion.</p> <p>Dataset S5. Measured and corrected trace element compositions of melt inclusion.</p> <p>Dataset S6. Pb isotopic compositions of melt inclusion.</p>

opencc-by-4.0Jun 2022View details →
zenodo36/100

Discovery of Ultra-depleted Melt Inclusion in Late Cretaceous Intraplate Basaltic Andesites in South China

<p>1. Suporting informations, including methods, figures, and one table.&nbsp;</p> <p>2. Six Datasets, including one dataset for basaltic rocks from different settings and five datasets for chemical and isotopic compositions of whole-rocks and melt inclusions.&nbsp;</p>

opencc-by-4.0Jun 2022View details →
zenodo36/100

Formation of ultra-depleted mantle peridotites and their relationship with boninitic melts: an example from the Kamuikotan Unit, Hokkaido, Japan

<p>Additional Supporting Information</p> <p>table_S1.xlsx: Compilation of the ultra-depleted peridotites<br> table_S1.xlsx: Locations and mineral major and trace elements compositions of the Takadomari and Horokanai ultra-depleted peridotites<br> table_S3.xlsx: Mineral and melt trace elements compositions obtained by our melting models</p> <p>QGIS<br> Geological map of the studied area</p>

opencc-by-4.0Oct 2022View details →
zenodo36/100

Discovery of Ultra-depleted Melt Inclusion in Late Cretaceous Intracontinental Basaltic Andesites in South China: Implications for Recycling of Lower Oceanic Crust

<p><strong>Contents of this file </strong></p> <p><strong>S1. Supplementary Text:</strong></p> <p><strong>1. </strong>Data compilation and statistical analysis</p> <p><strong>2.</strong> Reconstructing the chemical compositions of melt inclusion</p> <p><strong>3.</strong> Batch melting calculation</p> <p><strong>4.</strong> Melt-plagioclase diffusive interaction model</p> <p><strong>S2. Supplementary Table:</strong></p> <p><strong>Table S1. </strong>The parameters used in batch melting calculation.</p> <p><strong>Table S2. </strong>Parameters used in the melt-plagioclase diffusive interaction model</p> <p><strong>Table S3. </strong>Input and output data for the melt-plagioclase diffusive interaction model.</p> <p><strong>S3. Supplementary Figure:</strong></p> <p><strong>Figure S1. </strong>Primitive mantle-normalized trace element patterns.</p> <p><strong>S4. Supplementary Dataset (uploaded separately):</strong></p> <p><strong>Dataset S1. </strong>Compiled data including basaltic rocks from South China, MORBs, and Hawaiian OIBs.</p> <p><strong>Dataset S2. </strong>Olivine chemical compositions.</p> <p><strong>Dataset S3. </strong>Bulk-rock major oxide, trace element, and Sr-Nd-Pb-Hf isotopic compositions.</p> <p><strong>Dataset S4. </strong>Measured and corrected major element compositions of melt inclusion.</p> <p><strong>Dataset S5. </strong>Measured and corrected trace element compositions of melt inclusion.</p> <p><strong>Dataset S6. </strong>Pb isotopic compositions of melt inclusion.</p>

opencc-by-4.0Jul 2022View details →

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