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"Polarforschung"
Buggisch, W. , Bachtadse, V. and Paech, H. J.
(2001)
Paleomagnetic Investigations in Northeast Greenland and New Data from Devonian(?) and Late Carboniterous Rocks ,
Polarforschung,
Bremerhaven,
Alfred Wegener Institute for Polar and Marine Research & German Society of Polar Research,
69
,
pp. 55-64
.
hdl:10013/epic.29828
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"Polarforschung"
Höfle, H. C. and Buggisch, W.
(1995)
Glacial Geology and Petrography of Erratics in the Shackleton Range, Antarctica ,
Polarforschung,
Bremerhaven,
Alfred Wegener Institute for Polar and Marine Research & German Society of Polar Research,
63
(2/3),
pp. 183-201
.
hdl:10013/epic.29721
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"Polarforschung"
Buggisch, W. , Kleinschmidt, G. , Kreuzer, H. and Krumm, S.
(1994)
Metamorphic and Structural Evolution of the Southern Shackleton Range during the Ross Orogeny ,
Polarforschung,
Bremerhaven,
Alfred Wegener Institute for Polar and Marine Research & German Society of Polar Research,
63
(1),
pp. 33-56
.
hdl:10013/epic.29714
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"Polarforschung"
Kleinschmidt, G. and Buggisch, W.
(1994)
Plate Tectonic Implications of the Structure of the Shackleton Range, Antarctica ,
Polarforschung,
Bremerhaven,
Alfred Wegener Institute for Polar and Marine Research & German Society of Polar Research,
63
(1),
pp. 57-62
.
hdl:10013/epic.29715
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"Polarforschung"
Buggisch, W. , Kleinschmidt, G. , Höhndorf, A. and Pohl, J.
(1994)
Stratigraphy and Facies of Sediments and Low-grade Metasediments in the Shackleton Range, Antarctica ,
Polarforschung,
Bremerhaven,
Alfred Wegener Institute for Polar and Marine Research & German Society of Polar Research,
63
(1),
pp. 9-32
.
hdl:10013/epic.29713
|
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"Polarforschung"
Buggisch, W. , Piepjohn, K. , Thiedig, F. and von Gosen, W.
(1992)
A Middle Carboniferous Conodont Fauna from Blomstrandhalvoya (NW-Spitsbergen): Implications on the Age of Post-Devonian Karstification and the Svalbardian Deformation ,
Polarforschung,
Bremerhaven,
Alfred Wegener Institute for Polar and Marine Research & German Society of Polar Research,
62
(2/3),
pp. 83-90
.
hdl:10013/epic.29704
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