The Sidi Mohamed peridotites (Edough Massif, NE Algeria): Evidence for an upper mantle origin-Reference-Cited by-同舟云学术

The Sidi Mohamed peridotites (Edough Massif, NE Algeria): Evidence for an upper mantle origin

Published:2013-12 Issue:6 Volume:122 Page:1455-1465
ISSN:0253-4126
Container-title:Journal of Earth System Science
language:en
Short-container-title:J Earth Syst Sci

Author:

ZOBIR SORAYA HADJ,OBERHÄNSLI ROLAND

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/s12040-013-0358-z.pdf

Reference45 articles.

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3. Ahmed Said Y and Leake B E 1997 The petrogenesis of the Edough amphibolites, Annaba, NE Algeria: Two unrelated basic magmas and the lherzolite–harzburgite residue of a possible magma source; Mineral Petrol. 59(3–4) 207–237, doi: 10.1016/0899-5362(93)90027-N .

4. Arai S 1987 An estimation of the least depleted spinel peridotite on the basis of olivine-spinel mantle array; Neues Jahrb. Ž. Mineral. Monatsh. 8 347–354.

5. Bhattacharyya C 1971 An evaluation of the chemical distinctions between igneous and metamorphic orthopyroxènes; Am. Mineral. 56 499–506.

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