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Interaction between protokimberlite melts and mantle lithosphere:Evidence from mantle xenoliths from the Dalnyaya kimberlite pipe,Yakutia(Russia)

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Geoscience Frontiers 2017年第4期8卷 693-710页

作者： I.V.Ashchepkov t.ntaflos Z.V.Spetsius R.F.Salikhov H.Downes Institute of Geology and Mineralogy SD RAS Vienna University Alrosa Stock Company Department of Earth and Planetary Sciences Birkbeck University of London

the Dalnyaya kimberlite pipe（Yakutia,Russia） contains mantle peridotite xenoliths（mostly Iherzolites and harzburgites） that show both sheared porphyroclastic（deformed） and coarse granular textures,together with ilmenite and clinopyroxene *** peridotites contain high-temperature Fe-rich clinopyroxenes,sometimes associated with picroilmenites,which are products of interaction of the lithospheric mantle with protokimberlite related *** orthopyroxene-derived geotherm for the lithospheric mantle beneath Dalnyaya is stepped similar to that beneath the Udachnaya *** granular xenoliths fall on a geotherm of 35 mWm-2 whereas deformed varieties yield a 45 mWm-2）geotherm in the 2-7.5 GPa pressure *** chemistry of the constituent minerals including garnet,olivine and clinopyroxene shows trends of increasing Fe~#（=Fe/（Fe＋Mg））with decreasing *** may suggest that the interaction with fractionating protokimberlite melts occurred at different *** major mantle lithologies are distinguished by the trace element patterns of their constituent minerals,determined by ***,some clinopyroxenes and rare garnets are depleted in Ba,Sr,HFSE and MREE and represent relic lithospheric ***-fertilized garnet and clinopyroxene are more *** distribution of trace elements between garnet and clinopyroxene shows that the garnets dissolved primary orthopyroxene and *** high temperature clinopyroxenes related to the protokimberlite melts partially dissolved these *** show decreases in Ni and increases in Al,Ca and ti from Mg-rich varieties to the more Fe-rich,deformed and refertilized *** showing higher Fe~#（0.11-0.15） are found within intergrowths of low-Cr ilmenite-clinopyroxene-garnet related to the crystallization of protokimberlite melts in feeder *** P-f（O_2） diagrams,garnets and Cr-rich clinopyroxenes indicate reduced conditions at the base of the lithosphere at-5

关键词： Mantle xenoliths trace element Melt interaction Kimberlite Pyrope Cr-diopside

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Monomineral universal clinopyroxene and garnet barometers for peridotitic,eclogitic and basaltic systems

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Geoscience Frontiers 2017年第4期8卷 775-795页

作者： I.V.Ashchepkov t.ntaflos A.M.Logvinova Z.V.Spetsius H.Downes N.V.Vladykin V.S.Sobolev Institute of Geology and Mineralogy SB RAS Vienna University Alrosa Stock Company Department of Earth and Planetary Sciences Birkbeck University of London Institute of Geochemistry SD RAS

New versions of the universal Jd-Di exchange clinopyroxene barometer for peridotites,pyroxenites and eclogites,and also garnet barometer for eclogites and peridotites were *** were checked using large experimental data sets for eciogitic（~530） and peridotitic systems（〉650）.the precision of the universal Cpx barometer for peridotites based on Jd-Di exchange is close to Cr-tschermal

关键词： Clinopyroxene Barometer Peridotite Eclogite Kimberlite Garnet

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Alakit and Daldyn kimberlite fields,Siberia,Russia:two types of mantle sub-terranes beneath central Yakutia?

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Geoscience Frontiers 2017年第4期8卷 671-692页

作者： I.V.Ashchepkov A.M.Logvinova t.ntaflos N.V.Vladykin S.I.Kostrovitsky Z.Spetsius S.I.Mityukhin S.A.Prokopyev N.S.Medvedev H.Downes Institute of Geology and Mineralogy SD RAS Institute of Geochemistry SD RAS Dept.of Lithospheric Research University of Vienna Alrosa Stock Company Nikolaev Institute of Inorganic Chemistry 3 Department of Earth and Planetary Sciences Birkbeck University of London

Mineral data from Yakutian kimberlites allow reconstruction of the history of lithospheric *** occur in compositions of mantle pyropes and clinopyroxenes from large kimberlite pipes in the Alakit and Daldyn *** the Alakit ***-diopsides are alkaline,and Stykanskaya and some other pipes contain more sub-calcic pyropes and dunitic-type diamond inclusions,while in the Daldyn field harzburgitic pyropes are *** eclogitic diamond inclusions in the Alakit field are sharply divided in types and conditions,while in the Daldyn field they show varying compositions and often continuous Pressure-temperature（P-t） ranges with increasing Fe~# with decreasing *** Alakit,Crpargasites to richterites were found in all pipes,while in Daldyn,pargasites are rare Dalnyaya and Zarnitsa ***-diopsides from the Alakit region show higher levels of light Rare Earth Elements（LREE）and stronger REE-slopes,and enrichment in light Rare Earth Elements（LREE）,sometimes th-U,and small troughs in *** the Daldyn field,the High Field Strength Elements HFSE troughs are more common in clinopyroxenes with low REE abundances,while those from sheared and refertilized peridotites have smooth *** from Alakit show HREE minima,but those from Daldyn often have a trough at Yand high U and ***/O2 diagrams from both regions show similarities,suggesting similar layering and *** degree of metasomatism is often higher for pipes which show dispersion in P-Fe~# trends for *** the mantle beneath Udachnaya and Aykhal,pipes show 6-7 linear arrays of P-Fe~# in the lower part of the mantle section at 7.5-3.0 GPa,probably reflecting primary subduction *** the Sytykanskaya pipe,there are several horizons with opposite inclinations which reflect metasomatic *** high dispersion of the P—Fe~# trend indicating widespread metasomatism is associated with decreased diamond *** explanation of the differences in miner

关键词： thermobarometry Geochemistry Daldyn Alakit Craton Lithosphere

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the Sytykanskaya kimberlite pipe:Evidence from deep-seated xenoliths and xenocrysts for the evolution of the mantle beneath Alakit,Yakutia,Russia

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Geoscience Frontiers 2015年第5期6卷 687-714页

作者： I.V.Ashchepkov A.M.Logvinova L.F.Reimers t.ntaflos Z.V.Spetsius N.V.Vladykin H.Downes D.S.Yudin A.V.travin L.V.Makovchuk V.S.Palesskiy O.S.Khmel'nikova Institute of Geology and Mineralogy SB RAS Vienna University Alrosa Stock Company Institute of Geochemistry SB RAS Birkbeck College University of LondonUKMalet Street

Mantle xenoliths（>150） and concentrates from late autolithic breccia and porphyritic kimberlite from the Sytykanskaya pipe of the Alakit field（Yakutia） were analyzed by EPMA and LAM ICP *** P-tX-f（O2） diagrams minerals from xenoliths show widest variations,the trends P-Fe#-CaO,f（O2）for minerals from porphyric kimberlites are more stepped than for xenocrysts from *** PtX points mark moving for protokimberlites from the lithosphere base（7.5 GPa） to pyroxenite lens（5-3.5 GPa） accompanied by Cr increase by AFC and creation of two trends P-Fe#OI10-12%and13-15%.the Opx-Gar-based mantle geotherm in Alakit field is close to 35 mW/m2 at 65 GPa and 600 C near Moho was *** oxidation state for the megacrystalline ilmenites is lower for the metasomatic associations due to reduction of protokimberlites on peridotites than for uncontaminated varieties at the lithosphere *** inclined linear REE patterns with deep HFSE troughs for the parental melts of clinopyroxene and garnet xenocrysts from breccia were influenced by differentiated *** for metasomatic xenoliths reveal less inclined slopes without deep troughs in spider *** reveal S-shaped REE *** clinopyroxenes from graphite bearing Cr-websterites show inclined and inflected in Gd spectrums with LREE variations due to AFC *** for garnets display less inclined patterns and Ba-Sr troughs but enrichment in ***40Ar/39Ar ages for micas from the Alakit mantle xenoliths for disseminated phlogopites reveal Proterozoic（1154 Ma） age of metasomatism in early Rodinia *** glimmerites with richterite- like amphiboles mark1015 Ma plume event in Rodinia ***600-550 Ma stage manifests final Rodinia *** last 385 Ma metasomatism is protokimberlite-related.

关键词： Kimberlites Mantle lithosphere Mantle xenoliths th

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