Palynology of Permian shale, clay and sandstone clasts from the Basen till in northern Vestfjella, Dronning Maud Land

Research output: Contribution to journal › Journal article › Research › peer-review

Standard

Palynology of Permian shale, clay and sandstone clasts from the Basen till in northern Vestfjella, Dronning Maud Land. / SOFIE, LINDSTRÖM.

In: Antarctic Science, Vol. 17, No. 1, 2005, p. 87-96.

Research output: Contribution to journal › Journal article › Research › peer-review

Harvard

SOFIE, LINDSTRÖM 2005, 'Palynology of Permian shale, clay and sandstone clasts from the Basen till in northern Vestfjella, Dronning Maud Land', Antarctic Science, vol. 17, no. 1, pp. 87-96. https://doi.org/10.1017/s0954102005002476

APA

SOFIE, LINDSTRÖM. (2005). Palynology of Permian shale, clay and sandstone clasts from the Basen till in northern Vestfjella, Dronning Maud Land. Antarctic Science, 17(1), 87-96. https://doi.org/10.1017/s0954102005002476

Vancouver

SOFIE LINDSTRÖM. Palynology of Permian shale, clay and sandstone clasts from the Basen till in northern Vestfjella, Dronning Maud Land. Antarctic Science. 2005;17(1):87-96. https://doi.org/10.1017/s0954102005002476

Author

SOFIE, LINDSTRÖM. / Palynology of Permian shale, clay and sandstone clasts from the Basen till in northern Vestfjella, Dronning Maud Land. In: Antarctic Science. 2005 ; Vol. 17, No. 1. pp. 87-96.

Bibtex

@article{b631671023ae40098dfecff15a845bb5,
title = "Palynology of Permian shale, clay and sandstone clasts from the Basen till in northern Vestfjella, Dronning Maud Land",
abstract = "The palynological content of randomly collected sedimentary rock clasts from the till on the south-east slope of the Basen nunatak in northern Vestfjella in western Dronning Maud Land indicate that these sedimentary rocks were derived from strata of Middle Permian age. The palynological content and preservation is similar to palynofloras described from the sedimentary rocks that crop out at the Fossilryggen nunatak to the south-east, therefore, it seems likely that the Fossilryggen area represents the source of the sedimentary rock samples in the Basen till. This is further supported by known ice flow directions obtained from striations and clast fabric measurements in the area.",
author = "LINDSTR{\"O}M SOFIE",
year = "2005",
doi = "10.1017/s0954102005002476",
language = "English",
volume = "17",
pages = "87--96",
journal = "Antarctic Science",
issn = "0954-1020",
publisher = "Cambridge University Press",
number = "1",

}

RIS

TY - JOUR

T1 - Palynology of Permian shale, clay and sandstone clasts from the Basen till in northern Vestfjella, Dronning Maud Land

AU - SOFIE, LINDSTRÖM

PY - 2005

Y1 - 2005

N2 - The palynological content of randomly collected sedimentary rock clasts from the till on the south-east slope of the Basen nunatak in northern Vestfjella in western Dronning Maud Land indicate that these sedimentary rocks were derived from strata of Middle Permian age. The palynological content and preservation is similar to palynofloras described from the sedimentary rocks that crop out at the Fossilryggen nunatak to the south-east, therefore, it seems likely that the Fossilryggen area represents the source of the sedimentary rock samples in the Basen till. This is further supported by known ice flow directions obtained from striations and clast fabric measurements in the area.

AB - The palynological content of randomly collected sedimentary rock clasts from the till on the south-east slope of the Basen nunatak in northern Vestfjella in western Dronning Maud Land indicate that these sedimentary rocks were derived from strata of Middle Permian age. The palynological content and preservation is similar to palynofloras described from the sedimentary rocks that crop out at the Fossilryggen nunatak to the south-east, therefore, it seems likely that the Fossilryggen area represents the source of the sedimentary rock samples in the Basen till. This is further supported by known ice flow directions obtained from striations and clast fabric measurements in the area.

U2 - 10.1017/s0954102005002476

DO - 10.1017/s0954102005002476

M3 - Journal article

VL - 17

SP - 87

EP - 96

JO - Antarctic Science

JF - Antarctic Science

SN - 0954-1020

IS - 1

ER -

ID: 290451464