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Geology, geophysics, and hydrocarbon potential of Antarctica continental margin of Weddell Sea

Conference · · AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
OSTI ID:6220842
A prominent escarpment, called the Explora-Andenes Escarpment, has been recognized between long. 40/sup 0/W, lat. 72/sup 0/40'S and long. 10/sup 0/W, lat. 69/sup 0/20'S. It separates the continental margin from the Weddell Sea basin. Their recent MCS data have revealed the presence of some remarkably symmetric structures beneath a thick pile of tectonically undisturbed sediments. For example, two extensive wedge-shaped basement units occur between 20/sup 0/W and 40/sup 0/W. These units are characterized by a pattern of divergent reflectors which surround an elongated depression in basement. The northern wedge terminates against the Explora-Andenes Escarpment between 25/sup 0/W and 30/sup 0/W. The southern wedge, known as the Explora Wedge, shows a northward-dipping reflection pattern. The seismic characteristics suggest that both wedges consist of volcanic rocks. The basement depression is interpreted as a failed rift basin. The initial fragmentation of Gondwana was accompanied by prolific volcanism, which led to the emplacement of the wedges of dipping reflectors. The tectonomagmatic/volcanic period was followed by transtensional movements between Africa and Antarctica. This phase was heralded by the formation of the Explora-Andenes Escarpment as a new plate boundary and the opening of the Weddell Sea by sea-floor spreading. The Explora-Andenes Escarpment cuts across the early rift structures.
Research Organization:
Institute for Geosciences and Natural Resources, Hannover, West Germany
OSTI ID:
6220842
Report Number(s):
CONF-870606-
Conference Information:
Journal Name: AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States) Journal Volume: 71:5
Country of Publication:
United States
Language:
English

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