The late Proterozoic ophiolite of Sol Hamed, NE Sudan

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doi: 10.1016/0301-9268(83)90022-0
Authors:Fitches, W. R.; Graham, R. H.; Hussein, I. M.; Ries, Alison C.; Shackleton, R. M.; Price, R. C.
Author Affiliations:Primary:
University Coll. Wales, Aberystwyth SY23 2AX, United Kingdom
Other:
Univ. Coll. Swansea, United Kingdom
Minist. Energy Min., Sudan
Open Univ., United Kingdom
Volume Title:Precambrian Research
Source:Precambrian Research, 19(4), p.385-411. Publisher: Elsevier, Amsterdam, International. ISSN: 0301-9268
Publication Date:1983
Note:In English. 2 p. refs.; illus. incl. geol. sketch map
Summary:The Sol Hamed complex comprises ultramafic rocks, gabbros, sheeted dykes and pillow lavas and is an obducted, tilted ophiolite. It is unconformably overlain by the Nafirdeib series (712 + or - 58 m.y.) - a volcaniclastic series of conglomerates, olistostromes, felsitic and dacitic tuffs, turbidites, black shales and andesites; NE-SW folds and cleavage postdate the deposition of the series. Granite (approx 669 m.y.) intrudes the ophiolite and the Nafirdeib series. Averaged analyses (major and trace elements) are given for several basalts, andesites and dacites from different parts of the Nafirdeib series. The ophiolite is thought to occur on a suture, with the series representing part of an island-arc sequence. [A.C.B.]
Subjects:Carbonate rocks; Deformation; Gabbros; Igneous rocks; Lava; Limestone; Marine environment; Neoproterozoic; Olistostromes; Ophiolite; Petrology; Pillow lava; Plutonic rocks; Precambrian; Proterozoic; Provenance; Sedimentary rocks; Sedimentary structures; Sedimentation; Soft sediment deformation; Ultramafics; Unconformities; Upper Precambrian; Volcanic rocks; Africa; East Africa; Sudan; Environment; Nafirdeib Series; Sol Hamed
Coordinates:N213000 N223000 E0364500 E0360000
Abstract Numbers:84M/1046
Record ID:1985010001
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom, Reference includes data from PASCAL, Institute de l'Information Scientifique et Technique
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