_version_ 1867171777172471808
author Spaeth, Gerhard
Schüll, P
author_facet Spaeth, Gerhard
Schüll, P
collection Datos científicos de ciencias marinas y ambientales
contents In western Neuschwabenland basic dikes occur in the Jurassic lavas and Permian sediments of Vestfjella as weil as in the Precambrian sedimentary-volcanogenic rock sequence of the Ahlmannryggen and in the Precambrian crystalline complexes of Heimefrontfjella and Mannefallknausane. The concentration of the dikes in Vestfjella is conspicuous. Two main directions of strike perpendicular to each other are recognizable, from which the NE-SW striking one is predominant. The direction of the dikes coincides with the Mesozoic and younger fracture tectonics. Age relationships by structural, petrographical and geochemical observations are confirmed by palaeomagnetic and radiometrie age determinations from PETERS et al. (1986). Considerations on the geochemistry of further dolerite occurrences from Antarctica and other regions of the Gondwana continent are pointed out. Finally comparisons with the analogous South African dike system show the geotectonic significance of the dolerite dikes for the break-up of Gondwana.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_761606
institution PANGAEA
language en
publishDate 1987
publisher PANGAEA
record_format pangaea
spellingShingle Tab. 2: Average geochemical composition of dolerites from Neuschwabenland
Spaeth, Gerhard
Schüll, P
-; Ahlmannryggen; Ahlmannryggen, Neuschwabenland, Antarctica; Aluminium oxide; Barium; Calcium oxide; Calculated; Chromium; Cobalt; Event label; Heimefrontfjella; Heimefrontfjella, Antarctica; Iron oxide, Fe2O3; Loss on ignition; Magnesium oxide; Manganese oxide; Nickel; Phosphorus pentoxide; Potassium/Barium ratio; Potassium/Rubidium ratio; Potassium oxide; Rubidium; Silicon dioxide; Sodium oxide; Strontium; Titanium dioxide; Vanadium; Vestfjella; Vestfjella, Kraul Mountains, Neuschwabenland, Antarctica; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium
In western Neuschwabenland basic dikes occur in the Jurassic lavas and Permian sediments of Vestfjella as weil as in the Precambrian sedimentary-volcanogenic rock sequence of the Ahlmannryggen and in the Precambrian crystalline complexes of Heimefrontfjella and Mannefallknausane. The concentration of the dikes in Vestfjella is conspicuous. Two main directions of strike perpendicular to each other are recognizable, from which the NE-SW striking one is predominant. The direction of the dikes coincides with the Mesozoic and younger fracture tectonics. Age relationships by structural, petrographical and geochemical observations are confirmed by palaeomagnetic and radiometrie age determinations from PETERS et al. (1986). Considerations on the geochemistry of further dolerite occurrences from Antarctica and other regions of the Gondwana continent are pointed out. Finally comparisons with the analogous South African dike system show the geotectonic significance of the dolerite dikes for the break-up of Gondwana.
title Tab. 2: Average geochemical composition of dolerites from Neuschwabenland
topic -; Ahlmannryggen; Ahlmannryggen, Neuschwabenland, Antarctica; Aluminium oxide; Barium; Calcium oxide; Calculated; Chromium; Cobalt; Event label; Heimefrontfjella; Heimefrontfjella, Antarctica; Iron oxide, Fe2O3; Loss on ignition; Magnesium oxide; Manganese oxide; Nickel; Phosphorus pentoxide; Potassium/Barium ratio; Potassium/Rubidium ratio; Potassium oxide; Rubidium; Silicon dioxide; Sodium oxide; Strontium; Titanium dioxide; Vanadium; Vestfjella; Vestfjella, Kraul Mountains, Neuschwabenland, Antarctica; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium
url https://doi.org/10.1594/PANGAEA.761606