Continental breakup and the onset of ultraslow seafloor spreading off Flemish Cap on the Newfoundland rifted margin-Reference-Cited by-同舟云学术

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Continental breakup and the onset of ultraslow seafloor spreading off Flemish Cap on the Newfoundland rifted margin

Published:2004 Issue:1 Volume:32 Page:93
ISSN:0091-7613
Container-title:Geology
language:en
Short-container-title:Geol

Author:

Hopper John R.,Funck Thomas,Tucholke Brian E.,Christian Larsen Hans,Holbrook W. Steven,Louden Keith E.,Shillington Donna,Lau Helen

Publisher

Geological Society of America

Subject

Geology

Reference17 articles.

1. Gravity evidence of very thin crust at the Gakkel Ridge (Arctic Ocean)

2. Deep structure of the ocean-continent transition in the southern Iberia Abyssal Plain from seismic refraction profiles: The IAM-9 transect at 40°20′N

3. Patterns of continental extension along the conjugate margins of the central and North ATLANTIC Oceans and Labrador Sea

4. A Mesozoic time scale

5. The effect of lower crustal flow on continental extension and passive margin formation

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1. Magma-poor continent–ocean transition zones of the southern North Atlantic: a wide-angle seismic synthesis of a new frontier;Solid Earth;2024-06-21

2. Crustal structure of onshore-offshore Atlantic Canada and environs from constrained 3-D gravity inversion using variable mesh depths;Geophysical Journal International;2023-11-15

3. The crustal structure of the western Amundsen Basin, Arctic Ocean, derived from seismic refraction/wide-angle reflection data;Geophysical Journal International;2023-10-17

4. Linking rifted margin crustal shape with the timing and volume of magmatism;Terra Nova;2023-10-13

5. Structural configuration and tectonics of the Flemish Cap, offshore Newfoundland, from newly acquired seismic reflection data;Journal of the Geological Society;2023-06-15

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