The Sytykanskaya kimberlite pipe:Evidence from deep-seated xenoliths and xenocrysts for the evolution of the mantle beneath Alakit,Yakutia,Russia
The Sytykanskaya kimberlite pipe:Evidence from deep-seated xenoliths and xenocrysts for the evolution of the mantle beneath Alakit,Yakutia,Russia作者机构:Institute of Geology and Mineralogy SB RAS Vienna University Alrosa Stock Company Institute of Geochemistry SB RAS Birkbeck CollegeUniversity of LondonUKMalet Street
出 版 物:《Geoscience Frontiers》 (地学前缘(英文版))
年 卷 期:2015年第6卷第5期
页 面:687-714页
核心收录:
学科分类:070904[理学-构造地质学] 0709[理学-地质学] 07[理学]
基 金:supported by RBRF grants 05-05-64718,03-05-64146,08-05-00524,11-05-00060,11-05-91060-PICS jointresearch projects of IGM SB RAS and ALROSA Stock Company 77-2,65-03,02-05,grant of the President of Russia MK-3240.2014.5
主 题:Kimberlites Mantle lithosphere Mantle xenoliths Th
摘 要: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.