Is the Troodos Massif of Cyprus a Fragment of Mesozoic Ocean Floor? View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1968-10

AUTHORS

I. G. GASS

ABSTRACT

Available geological and geophysical data indicate that the Troodos massif is a Mesozoic volcanic complex the structure of which is comparable with that, deduced from geophysical data, for present day mid-ocean rises. It is suggested that the massif evolved beneath an oceanic Tethys and may represent a fragment of a mid-Tethyan rise. More... »

PAGES

39-42

Journal

TITLE

Nature

ISSUE

5162

VOLUME

220

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/220039a0

DOI

http://dx.doi.org/10.1038/220039a0

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1028708790


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