Publication Type:

Journal Article

Authors:

Stern, Robert J.; Ali, Kamal A.; Ren, Minghua; Jarrar, Ghaleb H.; Romer, Rolf L.; Leybourne, Matthew I.; Whitehouse, Martin J.; Ibrahim, Khalil M.

Source:

Earth and Planetary Science LettersEarth and Planetary Science Letters, Elsevier, Amsterdam, Netherlands, Volume 436, p.31-42 (2016)

ISBN:

0012-821X

Keywords:

absolute age, Africa, alkaline earth metals, Arabian Peninsula, Arabian Shield, Asia, asthenosphere, basalts, buried features, Cadomian Orogeny, Cenozoic, chemical composition, continental crust, crust, cumulates, dates, Gondwana, igneous rocks, inclusions, isotope ratios, Isotopes, Jordan, lower crust, metals, Middle East, mineral composition, Neogene, neoproterozoic, nesosilicates, Nubian Shield, orthosilicates, paleogeography, Precambrian, proterozoic, silicates, Sr-87/Sr-86, Stable isotopes, strontium, Tertiary, U/Pb, underplating, upper Precambrian, volcanic rocks, xenoliths, zircon, zircon group

Abstract:

In order to better understand the nature and formation of the lower continental crust beneath northern Arabia, we studied lower crustal xenoliths brought up by Neogene basalts in NE Jordan. Most of these xenoliths are comprised of primary phases plagioclase + two-pyroxenes with magnetite and ilmenite. Most clinopyroxene are augite whereas orthopyroxene mostly are hypersthene (Mg# = 50-80). Plagioclase feldspar is dominantly andesine-labradorite; pyrope-rich garnet and Fe-rich olivine (Fo (sub 75) to Fo (sub 62) ) are rare. These xenoliths represent cumulates formed from intermediate magmas that pooled in the lower crust. Many xenoliths also contain small, fine-grained K-rich zones interpreted as melt pockets reflecting late magmatic infiltration of the lower crust. The xenoliths display a wide range in major element compositions (37-51 wt.% SiO (sub 2) , 4-15 wt.% MgO and 0.1-6.3 wt.% TiO (sub 2) ), enrichment in Ba, K, Sr, Pb and Eu, and some trace element ratios atypical of bulk continental crust (e.g., K/Rb=1265+ or -565, K/U=63000+ or -60080 and Th/U=0.96+ or -0.56); these extreme ratios reflect widespread K-metasomatism associated with melt pockets. The magmas from which these cumulates formed may have been generated at a reararc convergent margin setting. Four U-Pb zircon populations yield indistinguishable ages of 554 + or -4 Ma; 559 + or -5 Ma; 559 + or -6 Ma, and 563 + or -5 Ma. Initial (super 87) Sr/ (super 86) Sr values (0.70260-0.70352) and positive epsilon Nd (sub (560)) (with the exception of a single, more radiogenic sample (+9.6), range=+1.3 to +4.8) indicate that the lower crust sampled by the xenoliths originated in the asthenospheric mantle, with little or no interaction with older crust, although Pb isotopic compositions allow for some interaction with older or subducted crustal materials. We interpret the geochemistry and mineralogy of these xenoliths to indicate that the lower crust beneath NE Jordan is mafic and comprised of plagioclase-rich 2-pyroxene igneous rocks. The lower crust of this area formed by magmatic underplating over less than 18 Ma. The crust of NE Jordan is significantly younger than the crust of the northernmost Arabian-Nubian Shield and represents a fragment of Cadomian (600-520 Ma) crust that may make up the NE margin of the Arabian Plate. Abstract Copyright (2016) Elsevier, B.V.

Notes:

GeoRef, Copyright 2018, American Geological Institute.<br/>2016-046578