Lower Paleozoic oceanic crust in Mongolian Caledonides: SM-ND isotope and trace element data

Mongolian ophiolites range in age from Early Proterozoic to Middle Paleozoic with maximum of ophiolite production in Late Riphean to Early Cambrian time. One of the best examples is the Bayan‐Khongor complex which comprise serpentinized peridotite, cumulate sequence, sheeted dike unit and metavolcan...

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Veröffentlicht in:	Geophysical research letters 1991-07, Vol.18 (7), p.1301-1304
Hauptverfasser:	Kepezhinskas, P. K., Kepezhinskas, K. B., Pukhtel, I. S.
Format:	Artikel
Sprache:	eng
Schlagworte:	Age Basins Dikes Gabbro Marine Origins Ridges Segments Spreading
Online-Zugang:	Volltext
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