Newtontoppen granitoid rocks, their geology, chemistry and Rb-Sr age

• Published in: Polar Research
• Main Authors: Teben'kov, A. M., Ohta, Y., Balašov, Ju. A., Sirotkin, A. N.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Norwegian Polar Institute 1996
• Subjects: Sickle; Ny Friesland; Newtontoppen; Chydeniusbreen; Ekkoknausane; Polar Research
• Online Access: https://polarresearch.net/index.php/polar/article/view/1920; https://doi.org/10.3402/polar.v15i1.6637

A post-tectonic Caledonian granite in southern Ny Friesland has been fully mapped and the following new names are proposed: the Chydeniusbreen granitoid suite, consisting of the Raudberget granitoid body in the north; the Newtontoppen granitoid body in the middle; and the Ekkoknausane granitoid body in the south The contact relationships, internal structures and distribution of various rock types infer an asymmetric lopolith or a harpolith-like body, a large sickle-shaped intrusion stretched in the direction of general tectonic transport, for the Newtontoppen granitoid body. Seven rock types are described in the Newtontoppen granitoid and four emplacement stages are recognised. The major rock types seem to have an alkali-calcic to alkalic bulk rock chemistry and show a transition between I- and S-type granite derived from anatectic melting of various protoliths under relatively high temperature conditions. Possible later K20 introduction modified the earlier formed rock types. A Rb-Sr whole rock age of 432 ± 10 Ma has been obtained by a seven point isochron with MSDW = 2.59 and an initial Sr isotope ratio = 0.715. This age is approximately 30 Ma older than the previously obtained K-Ar whole rock and Rb-Sr biotite ages, ca. 400 Ma, which represents the period of cooling. The high initial Sr isotope ratio supports the interpretation of an anatectic origin.