Seismic structure of the St. Paul Fracture Zone and Late Cretaceous to Mid Eocene oceanic crust in the equatorial Atlantic Ocean near 18°W-Reference-Cited by-同舟云学术

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Seismic structure of the St. Paul Fracture Zone and Late Cretaceous to Mid Eocene oceanic crust in the equatorial Atlantic Ocean near 18°W

Published:2021-09-27 Issue: Volume: Page:
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Author:

Growe Kevin¹^ORCID,Grevemeyer Ingo¹^ORCID,Singh Satish Chandra²^ORCID,Marjanovic Milena²^ORCID,Gregory Emma PM²^ORCID,Papenberg Cord³^ORCID,Vaddineni Venkata Abhishikth²,Gómez de la Peña Laura⁴^ORCID,Wang Zhikai²^ORCID

Affiliation:

1. GEOMAR Helmholtz Centre for Ocean Research Kiel

2. Institut De Physique Du Globe De Paris

3. Geomar, Kiel, Germany

4. GEOMAR Helmholtz Centre of Ocean Research

Funder

European Research Council

Publisher

Wiley

Reference5 articles.

1. Oceanographer transform fault structure compared to that of surrounding oceanic crust: Results from seismic refraction data analysis;Ambos E.L;Journal of geodynamics,1986

2. Crustal control of ridge segmentation inferred from observations of the Reykjanes Ridge;Bell R. E.;Nature,1992

3. Bird P. (2003). "An updated digital model of plate boundaries". Geochemistry Geophysics Geosystems 4.3. https://doi.org/10.1029/2001GC000252

4. A cold suboceanic mantle belt at the Earth equator;Bonatti E.;Science,1993

5. Cannat M. (1993). Emplacement of mantle rocks in the seafloor at mid ocean ridges ---------- Journal of Geophysical Research 98 4163-4172. https://doi.org/10.1029/92JB02221 838 839 840 841 842 843 844 845 846 847 848

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