Diagrammatic Representation of the Geology in the Dry Valleys, McMurdo Sound, Antarctica. — FIG. 1: Deposition of Skelton Group sediments in a geosyncline of Precambrian to Cambrian age, with subsequent igneous intrusion. — FIG. 2: Ordovician Orogeny — folding and metamorphism of the sediments with contemporaneous intrusion of a syntectonic granodiorite batholith (crosses a). Post-tectonic intrusion of a granite of sheet-like form (carets b), with lamprophyre and porphyry dykes of two generations (black lines)

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Subjects:
McMurdo Sound
Antarc*
Antarctica
Online Access:http://www.nzetc.org/tm/scholarly/Bio15Tuat03-fig-Bio15Tuat03_121a.html
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spelling ftnzetc:oai:nzetc.org:Bio15Tuat03-fig-Bio15Tuat03_121a 2024-04-14T08:01:52+00:00 Diagrammatic Representation of the Geology in the Dry Valleys, McMurdo Sound, Antarctica. — FIG. 1: Deposition of Skelton Group sediments in a geosyncline of Precambrian to Cambrian age, with subsequent igneous intrusion. — FIG. 2: Ordovician Orogeny — folding and metamorphism of the sediments with contemporaneous intrusion of a syntectonic granodiorite batholith (crosses a). Post-tectonic intrusion of a granite of sheet-like form (carets b), with lamprophyre and porphyry dykes of two generations (black lines) text/html http://www.nzetc.org/tm/scholarly/Bio15Tuat03-fig-Bio15Tuat03_121a.html unknown http://www.nzetc.org/tm/scholarly/Bio15Tuat03-fig-Bio15Tuat03_121a.html StillImage ftnzetc 2024-03-18T10:42:16Z Still Image Antarc* Antarctica McMurdo Sound New Zealand Electronic Text Collection (Victoria University of Wellington) McMurdo Sound
institution Open Polar
collection New Zealand Electronic Text Collection (Victoria University of Wellington)
op_collection_id ftnzetc
language unknown
format Still Image
title Diagrammatic Representation of the Geology in the Dry Valleys, McMurdo Sound, Antarctica. — FIG. 1: Deposition of Skelton Group sediments in a geosyncline of Precambrian to Cambrian age, with subsequent igneous intrusion. — FIG. 2: Ordovician Orogeny — folding and metamorphism of the sediments with contemporaneous intrusion of a syntectonic granodiorite batholith (crosses a). Post-tectonic intrusion of a granite of sheet-like form (carets b), with lamprophyre and porphyry dykes of two generations (black lines)
spellingShingle Diagrammatic Representation of the Geology in the Dry Valleys, McMurdo Sound, Antarctica. — FIG. 1: Deposition of Skelton Group sediments in a geosyncline of Precambrian to Cambrian age, with subsequent igneous intrusion. — FIG. 2: Ordovician Orogeny — folding and metamorphism of the sediments with contemporaneous intrusion of a syntectonic granodiorite batholith (crosses a). Post-tectonic intrusion of a granite of sheet-like form (carets b), with lamprophyre and porphyry dykes of two generations (black lines)
title_short Diagrammatic Representation of the Geology in the Dry Valleys, McMurdo Sound, Antarctica. — FIG. 1: Deposition of Skelton Group sediments in a geosyncline of Precambrian to Cambrian age, with subsequent igneous intrusion. — FIG. 2: Ordovician Orogeny — folding and metamorphism of the sediments with contemporaneous intrusion of a syntectonic granodiorite batholith (crosses a). Post-tectonic intrusion of a granite of sheet-like form (carets b), with lamprophyre and porphyry dykes of two generations (black lines)
title_full Diagrammatic Representation of the Geology in the Dry Valleys, McMurdo Sound, Antarctica. — FIG. 1: Deposition of Skelton Group sediments in a geosyncline of Precambrian to Cambrian age, with subsequent igneous intrusion. — FIG. 2: Ordovician Orogeny — folding and metamorphism of the sediments with contemporaneous intrusion of a syntectonic granodiorite batholith (crosses a). Post-tectonic intrusion of a granite of sheet-like form (carets b), with lamprophyre and porphyry dykes of two generations (black lines)
title_fullStr Diagrammatic Representation of the Geology in the Dry Valleys, McMurdo Sound, Antarctica. — FIG. 1: Deposition of Skelton Group sediments in a geosyncline of Precambrian to Cambrian age, with subsequent igneous intrusion. — FIG. 2: Ordovician Orogeny — folding and metamorphism of the sediments with contemporaneous intrusion of a syntectonic granodiorite batholith (crosses a). Post-tectonic intrusion of a granite of sheet-like form (carets b), with lamprophyre and porphyry dykes of two generations (black lines)
title_full_unstemmed Diagrammatic Representation of the Geology in the Dry Valleys, McMurdo Sound, Antarctica. — FIG. 1: Deposition of Skelton Group sediments in a geosyncline of Precambrian to Cambrian age, with subsequent igneous intrusion. — FIG. 2: Ordovician Orogeny — folding and metamorphism of the sediments with contemporaneous intrusion of a syntectonic granodiorite batholith (crosses a). Post-tectonic intrusion of a granite of sheet-like form (carets b), with lamprophyre and porphyry dykes of two generations (black lines)
title_sort diagrammatic representation of the geology in the dry valleys, mcmurdo sound, antarctica. — fig. 1: deposition of skelton group sediments in a geosyncline of precambrian to cambrian age, with subsequent igneous intrusion. — fig. 2: ordovician orogeny — folding and metamorphism of the sediments with contemporaneous intrusion of a syntectonic granodiorite batholith (crosses a). post-tectonic intrusion of a granite of sheet-like form (carets b), with lamprophyre and porphyry dykes of two generations (black lines)
url http://www.nzetc.org/tm/scholarly/Bio15Tuat03-fig-Bio15Tuat03_121a.html
geographic McMurdo Sound
geographic_facet McMurdo Sound
genre Antarc*
Antarctica
McMurdo Sound
genre_facet Antarc*
Antarctica
McMurdo Sound
op_relation http://www.nzetc.org/tm/scholarly/Bio15Tuat03-fig-Bio15Tuat03_121a.html
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