About This Item

Share This Item

The AAPG/Datapages Combined Publications Database

AAPG Bulletin

Abstract


Volume: 61 (1977)

Issue: 9. (September)

First Page: 1483

Last Page: 1492

Title: Continental Slope and Upper Rise off Western Nova Scotia and Georges Bank

Author(s): Elazar Uchupi, R. D. Ballard, J. P. Ellis (2)

Abstract:

The continental margin from western Nova Scotia to the western edge of Georges Bank consists of two sedimentary wedges, one beneath the shelf and the other beneath the continental rise. Most of the upper rise sequence was deposited by turbidity currents modified to some extent by bottom currents. Off Nova Scotia, vertical migration of salt has formed a ridge along the entire length of the Nova Scotia Rise. The diapiric ridge terminates southwestward against a basement high beneath the continental slope south of Georges Bank. This basement high initially blocked the southwestern flow of the invading Tethys sea, but as the Atlantic basin continued to widen and deepen, the high was breached and evaporite deposition ceased.

Pay-Per-View Purchase Options

The article is available through a document delivery service. Explain these Purchase Options.

Watermarked PDF Document: $14
Open PDF Document: $24

AAPG Member?

Please login with your Member username and password.

Members of AAPG receive access to the full AAPG Bulletin Archives as part of their membership. For more information, contact the AAPG Membership Department at [email protected].