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(PDF) Ancient sub-continental lithospheric mantle (SCLM) beneath the eastern part of the Central Asian Orogenic Belt (CAOB): Implications for crust–mantle decoupling | Zhu-Yin Chu - Academia.edu

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{"work":{"id":93820502,"created_at":"2022-12-27T16:45:52.463-08:00","from_world_paper_id":223915510,"updated_at":"2024-11-27T02:49:25.254-08:00","_data":{"publisher":"Elsevier BV","grobid_abstract":"Potassic basaltic lavas erupted during the Cenzoic are widespread in Wudalianchi, Erkeshan and Keluo (WEK) areas, northeast China, and contain abundant mantle xenoliths. Mantle xenoliths in this study are selected from the Keluo potassic lavas, and mainly comprise spinel lherzolites and harzburgites with minor dunites and wehrlites. Modal metasomatism is evident in some Keluo xenoliths from the presence of phlogopite and rutile. Mineral compositions indicate that the Keluo xenoliths represent mantle residues after variable degrees of melting, i.e., 1-5% for lherzolites and 3-11% for harzburgites, with subsequent refertilization. Both bulk-rock and clinopyroxene data show enrichment in light rare earth elements (LREE) and some other incompatible elements (e.g. Ba, U). Clinopyroxenes from some of the Keluo xenoliths have radiogenic Sr isotopes, but unradiogenic Nd-Hf isotopes relative to the Cenozoic mantle xenoliths from other localities of the NE China. The Keluo mantle xenoliths have variable 187 Os/ 188 Os ratios ranging from 0.11458 to 0.13194. Although most Keluo mantle xenoliths have been affected by Re addition, their Os isotope compositions have not been significantly modified. The unradiogenic 187 Os/ 188 Os ratios of the refractory harzburgites give Re depletion ages (T RD) of~1.9-2.1 Ga. This suggests that the sub-continental lithospheric mantle (SCLM) beneath the Keluo area was formed during the Paleoproterozoic, which is older than the age of the overlying crust that was mainly formed since the Neoproterozoic. Therefore, the SCLM beneath the Kelou area is temporally decoupled from the overlying crust. It is unlikely that the Cenozoic SCLM beneath the Keluo area was newly accreted from the asthenosphere, in which ancient mantle domains were preserved. We propose that the ancient mantle beneath the Keluo region is extraneous and has been emplaced from other locations.","publication_date":"2011,,","publication_name":"Lithos","grobid_abstract_attachment_id":"96451882"},"document_type":"paper","pre_hit_view_count_baseline":null,"quality":"high","language":"en","title":"Ancient sub-continental lithospheric mantle (SCLM) beneath the eastern part of the Central Asian Orogenic Belt (CAOB): Implications for crust–mantle decoupling","broadcastable":false,"draft":null,"has_indexable_attachment":true,"indexable":true}}["work"]; window.loswp.workCoauthors = [53010234]; window.loswp.locale = "en"; window.loswp.countryCode = "SG"; window.loswp.cwvAbTestBucket = ""; window.loswp.designVariant = "ds_vanilla"; window.loswp.fullPageMobileSutdModalVariant = "full_page_mobile_sutd_modal"; window.loswp.useOptimizedScribd4genScript = false; window.loswp.appleClientId = 'edu.academia.applesignon';</script><script defer="" 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src="//a.academia-assets.com/images/s65_no_pic.png" />Zhu-Yin Chu</a></div><div class="ds-work-card--detail"><p class="ds-work-card--detail ds2-5-body-sm">2011, Lithos</p></div><div class="ds-work-card--button-container"><button class="ds2-5-button js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;continue-reading-button--work-card&quot;,&quot;attachmentId&quot;:96451882,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;workUrl&quot;:&quot;https://www.academia.edu/93820502/Ancient_sub_continental_lithospheric_mantle_SCLM_beneath_the_eastern_part_of_the_Central_Asian_Orogenic_Belt_CAOB_Implications_for_crust_mantle_decoupling&quot;}">See full PDF</button><button class="ds2-5-button ds2-5-button--secondary js-swp-download-button" 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ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Remnants of oceanic lower crust in the subcontinental lithospheric mantle: Trace element and Sr–Nd–O isotope evidence from aluminous garnet pyroxenite xenoliths from Jiaohe, Northeast China&quot;,&quot;attachmentId&quot;:45079229,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/13671181/Remnants_of_oceanic_lower_crust_in_the_subcontinental_lithospheric_mantle_Trace_element_and_Sr_Nd_O_isotope_evidence_from_aluminous_garnet_pyroxenite_xenoliths_from_Jiaohe_Northeast_China&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/13671181/Remnants_of_oceanic_lower_crust_in_the_subcontinental_lithospheric_mantle_Trace_element_and_Sr_Nd_O_isotope_evidence_from_aluminous_garnet_pyroxenite_xenoliths_from_Jiaohe_Northeast_China"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="6" data-entity-id="93820481" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/93820481/Mesozoic_accretion_of_juvenile_sub_continental_lithospheric_mantle_beneath_South_China_and_its_implications_Geochemical_and_Re_Os_isotopic_results_from_Ningyuan_mantle_xenoliths">Mesozoic accretion of juvenile sub-continental lithospheric mantle beneath South China and its implications: Geochemical and Re–Os isotopic results from Ningyuan mantle xenoliths</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="53010234" href="https://independent.academia.edu/ZhuYinChu">Zhu-Yin Chu</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Chemical Geology, 2012</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Mesozoic accretion of juvenile sub-continental lithospheric mantle beneath South China and its implications: Geochemical and Re–Os isotopic results from Ningyuan mantle xenoliths&quot;,&quot;attachmentId&quot;:96451871,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/93820481/Mesozoic_accretion_of_juvenile_sub_continental_lithospheric_mantle_beneath_South_China_and_its_implications_Geochemical_and_Re_Os_isotopic_results_from_Ningyuan_mantle_xenoliths&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/93820481/Mesozoic_accretion_of_juvenile_sub_continental_lithospheric_mantle_beneath_South_China_and_its_implications_Geochemical_and_Re_Os_isotopic_results_from_Ningyuan_mantle_xenoliths"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="7" data-entity-id="93820498" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/93820498/The_Xinchang_peridotite_xenoliths_reveal_mantle_replacement_and_accretion_in_southeastern_China">The Xinchang peridotite xenoliths reveal mantle replacement and accretion in southeastern China</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="53010234" href="https://independent.academia.edu/ZhuYinChu">Zhu-Yin Chu</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Lithos, 2012</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;The Xinchang peridotite xenoliths reveal mantle replacement and accretion in southeastern China&quot;,&quot;attachmentId&quot;:96451879,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/93820498/The_Xinchang_peridotite_xenoliths_reveal_mantle_replacement_and_accretion_in_southeastern_China&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/93820498/The_Xinchang_peridotite_xenoliths_reveal_mantle_replacement_and_accretion_in_southeastern_China"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="8" data-entity-id="13671243" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/13671243/Contrasting_Cenozoic_Lithospheric_Evolution_and_Architecture_in_the_Western_and_Eastern_Sino_Korean_Craton_Constraints_from_Geochemistry_of_Basalts_and_Mantle_Xenoliths">Contrasting Cenozoic Lithospheric Evolution and Architecture in the Western and Eastern Sino‐Korean Craton: Constraints from Geochemistry of Basalts and Mantle Xenoliths</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="32817976" href="https://gig.academia.edu/YigangXu">Yi-gang Xu</a></div><p class="ds-related-work--metadata ds2-5-body-xs">The Journal of Geology, 2004</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Contrasting Cenozoic Lithospheric Evolution and Architecture in the Western and Eastern Sino‐Korean Craton: Constraints from Geochemistry of Basalts and Mantle Xenoliths&quot;,&quot;attachmentId&quot;:45079170,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/13671243/Contrasting_Cenozoic_Lithospheric_Evolution_and_Architecture_in_the_Western_and_Eastern_Sino_Korean_Craton_Constraints_from_Geochemistry_of_Basalts_and_Mantle_Xenoliths&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/13671243/Contrasting_Cenozoic_Lithospheric_Evolution_and_Architecture_in_the_Western_and_Eastern_Sino_Korean_Craton_Constraints_from_Geochemistry_of_Basalts_and_Mantle_Xenoliths"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="9" data-entity-id="41456533" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/41456533/Reworking_of_old_continental_lithosphere_Unradiogenic_Os_and_decoupled_Hf_Nd_isotopes_in_sub_arc_mantle_pyroxenites">Reworking of old continental lithosphere: Unradiogenic Os and decoupled Hf-Nd isotopes in sub-arc mantle pyroxenites</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="141118519" href="https://independent.academia.edu/BenatOliveira">Benat Oliveira</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="10246740" href="https://omp.academia.edu/MichelGregoire">Michel Gregoire</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Lithos, 2019</p><p class="ds-related-work--abstract ds2-5-body-sm">Mantle lithologies in orogenic massifs and xenoliths commonly display strikingly different Hf- and Nd-isotope compositions compared to oceanic basalts. While the presence of pyroxenites has long been suggested in the source region of mantle-derived magmas, very few studies have reported their combined Hf\ \Nd isotope compositions.We here report the first Lu\ \Hf data along with Re\Os data and S concentrations on the Cabo Ortegal Complex,where the pyroxenite-rich Herbeira massif has been interpreted as remnants of a delaminated arc root. The pyroxenites, chromitites and their host harzburgites show a wide range of whole-rock 187Re/188Os and 187Os/188Os (0.16–1.44), indicating that Re was strongly mobilized, partly during hydrous retrograde metamorphism but mostly during supergene alteration that preferentially affected low Mg#, low Cu/S pyroxenites. Samples that escaped this disturbance yield an isochron age of 838 ± 42 Ma, interpreted as the formation of Cabo Ortegal pyroxenites. Corresponding values of initial 187Os/188Os (0.111–0.117) are relatively unradiogenic, suggesting limited contributions of slab-derived Os to primitive arc melts such as those parental to these pyroxenites. This interpretation is consistent with radiogenic Os in arc lavas being mostly related to crustal assimilation. Paleoproterozoic to Archean Os model ages confirm that Cabo Ortegal pyroxenites record incipient volcanic arc magmatism on the continental margin of the Western African Craton, as notably documented by zircon U\ \Pb ages of 2.1 and 2.7 Ga. Lu\ \Hf data collected on clinopyroxene and amphibole separates and whole rock samples are characterized by uncorrelated 176Lu/177Hf and 176Hf/177Hf (0.2822–0.2855), decoupled from Nd-isotope compositions. This decoupling is ascribed to diffusional disequilibrium during melt-peridotite interaction, in good agreement with the results of percolation-diffusion models simulating the interaction of an arc melt with an ancient melt-depleted residue. These models notably show that Hf\ \Nd isotopic decoupling such as recorded by Cabo Ortegal pyroxenites and peridotites (ΔƐHf(i) up to +97) is enhanced during melt peridotite interaction by slow diffusional re-equilibration and can be relatively insensitive to chromatographic fractionation. Finally, we discuss the hypothesis that arc-continent interaction may provide preferential conditions for such isotopic decoupling and propose that its ubiquitous recognition in peridotites reflects the recycling of sub-arc mantle domains derived from ancient, reworked SCLM.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Reworking of old continental lithosphere: Unradiogenic Os and decoupled Hf-Nd isotopes in sub-arc mantle pyroxenites&quot;,&quot;attachmentId&quot;:61730327,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/41456533/Reworking_of_old_continental_lithosphere_Unradiogenic_Os_and_decoupled_Hf_Nd_isotopes_in_sub_arc_mantle_pyroxenites&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/41456533/Reworking_of_old_continental_lithosphere_Unradiogenic_Os_and_decoupled_Hf_Nd_isotopes_in_sub_arc_mantle_pyroxenites"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div></div></div><div class="ds-sticky-ctas--wrapper js-loswp-sticky-ctas hidden"><div class="ds-sticky-ctas--grid-container"><div class="ds-sticky-ctas--container"><button class="ds2-5-button js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;continue-reading-button--sticky-ctas&quot;,&quot;attachmentId&quot;:96451882,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;workUrl&quot;:null}">See full PDF</button><button class="ds2-5-button ds2-5-button--secondary js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;download-pdf-button--sticky-ctas&quot;,&quot;attachmentId&quot;:96451882,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;workUrl&quot;:null}"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span>Download PDF</button></div></div></div><div class="ds-below-fold--grid-container"><div class="ds-work--container js-loswp-embedded-document"><div class="attachment_preview" data-attachment="Attachment_96451882" style="display: none"><div class="js-scribd-document-container"><div class="scribd--document-loading js-scribd-document-loader" style="display: block;"><img alt="Loading..." src="//a.academia-assets.com/images/loaders/paper-load.gif" /><p>Loading Preview</p></div></div><div style="text-align: center;"><div class="scribd--no-preview-alert js-preview-unavailable"><p>Sorry, preview is currently unavailable. You can download the paper by clicking the button above.</p></div></div></div></div><div class="ds-sidebar--container js-work-sidebar"><div class="ds-related-content--container"><h2 class="ds-related-content--heading">Related papers</h2><div class="ds-related-work--container js-related-work-sidebar-card" data-collection-position="0" data-entity-id="13671226" data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/13671226/Late_Archean_to_Early_Proterozoic_lithospheric_mantle_beneath_the_western_North_China_craton_Sr_Nd_Os_isotopes_of_peridotite_xenoliths_from_Yangyuan_and_Fansi">Late Archean to Early Proterozoic lithospheric mantle beneath the western North China craton: Sr–Nd–Os isotopes of peridotite xenoliths from Yangyuan and Fansi</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="32817976" 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Xinjiang, NW China: Implications for petrogenesis and Phanerozoic continental growth</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="26312811" href="https://cug.academia.edu/TimothyKusky">Timothy Kusky</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Lithos, 2012</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Geochronology and geochemistry of the Chuanwulu complex in the South Tianshan, western Xinjiang, NW China: Implications for petrogenesis and Phanerozoic continental growth&quot;,&quot;attachmentId&quot;:36753686,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/10823271/Geochronology_and_geochemistry_of_the_Chuanwulu_complex_in_the_South_Tianshan_western_Xinjiang_NW_China_Implications_for_petrogenesis_and_Phanerozoic_continental_growth&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-related-work-grid-card-view-pdf" href="https://www.academia.edu/10823271/Geochronology_and_geochemistry_of_the_Chuanwulu_complex_in_the_South_Tianshan_western_Xinjiang_NW_China_Implications_for_petrogenesis_and_Phanerozoic_continental_growth"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-related-work-sidebar-card" data-collection-position="3" data-entity-id="29777801" data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/29777801/Compositional_heterogeneity_of_the_continental_lithospheric_mantle_beneath_the_Early_Precambrian_and_Phanerozoic_structures_Evidence_from_mantle_xenoliths_in_kimberlites_and_alkaline_basalts">Compositional heterogeneity of the continental lithospheric mantle beneath the Early Precambrian and Phanerozoic structures: Evidence from mantle xenoliths in kimberlites and alkaline basalts</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="4208971" href="https://independent.academia.edu/IgorAshchepkov">Igor Ashchepkov</a><span>, </span><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="56727508" href="https://independent.academia.edu/NikitinaL">L. P Nikitina</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Geochemistry International, 2007</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Compositional heterogeneity of the continental lithospheric mantle beneath the Early Precambrian and Phanerozoic structures: Evidence from mantle xenoliths in kimberlites and alkaline basalts&quot;,&quot;attachmentId&quot;:50230359,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/29777801/Compositional_heterogeneity_of_the_continental_lithospheric_mantle_beneath_the_Early_Precambrian_and_Phanerozoic_structures_Evidence_from_mantle_xenoliths_in_kimberlites_and_alkaline_basalts&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" 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data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/90178609/A_refined_model_for_lithosphere_evolution_beneath_the_decratonized_northeastern_North_China_Craton">A refined model for lithosphere evolution beneath the decratonized northeastern North China Craton</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="92262997" href="https://independent.academia.edu/HongkunDai">Hongkun Dai</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Contributions to Mineralogy and Petrology, 2019</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;A refined model for lithosphere evolution beneath the decratonized northeastern North China 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data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/93820237/Source_of_highly_potassic_basalts_in_northeast_China_Evidence_from_Re_Os_Sr_Nd_Hf_isotopes_and_PGE_geochemistry">Source of highly potassic basalts in northeast China: Evidence from Re–Os, Sr–Nd–Hf isotopes and PGE geochemistry</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="53010234" href="https://independent.academia.edu/ZhuYinChu">Zhu-Yin Chu</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Chemical Geology, 2013</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Source of highly potassic basalts in northeast China: Evidence from Re–Os, Sr–Nd–Hf isotopes 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data-entity-id="90178509" data-sort-order="default"><a class="ds-related-work--title js-related-work-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/90178509/Mantle_xenoliths_and_host_basalts_record_the_Paleo_Asian_oceanic_materials_in_the_mantle_wedge_beneath_northwest_North_China_Craton">Mantle xenoliths and host basalts record the Paleo-Asian oceanic materials in the mantle wedge beneath northwest North China Craton</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="92262997" href="https://independent.academia.edu/HongkunDai">Hongkun Dai</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Solid Earth Sciences, 2019</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Mantle xenoliths and 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evolution</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="39679080" href="https://independent.academia.edu/KuidongZhao">Kui-dong Zhao</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Lithos, 2008</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Geochronology, geochemistry and Hf–Sr–Nd isotopic compositions of Huziyan mafic xenoliths, southern Hunan Province, South China: Petrogenesis and implications for lower crust 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peridotite xenoliths from Yantai, Shandong Province: Evidence for Phanerozoic lithospheric mantle beneath eastern North China Craton</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="32894924" href="https://independent.academia.edu/FengWang14">Feng Wang</a><span>, </span><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="32817976" href="https://gig.academia.edu/YigangXu">Yi-gang Xu</a></div><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Petrology, geochemistry and Re–Os isotopes of peridotite xenoliths from Yantai, Shandong Province: Evidence for Phanerozoic lithospheric mantle beneath eastern North China 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class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="35541998" href="https://independent.academia.edu/JeanyvesCottin">Jean-yves Cottin</a><span>, </span><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="32803471" href="https://independent.academia.edu/NMattielli">N. 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orogenic belt</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="47122534" href="https://hku-hk.academia.edu/GZhao">赵国春 Guochun Zhao</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Gondwana Research, 2012</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Carboniferous mantle-derived felsic intrusion in the Chinese Altai, NW China: Implications for geodynamic change of the accretionary orogenic 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contents and Sr-Nd isotope compositions for clinopyroxenes from peridotite xenoliths hosted by Cenozoic basalts</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="285185" href="https://zju.academia.edu/yantaoHao">yantao Hao</a></div><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Recognizing juvenile and relict lithospheric mantle beneath the North China Craton: Combined analysis of H2O and element contents and Sr-Nd isotope compositions for clinopyroxenes from peridotite xenoliths hosted by Cenozoic 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