Crustal Structure at a Young Continental Rift: A Receiver Function Study From the Tanganyika Rift-Reference-Cited by-同舟云学术

Crustal Structure at a Young Continental Rift: A Receiver Function Study From the Tanganyika Rift

Author:

Hodgson Isabel¹,Illsley-Kemp Finnigan¹^ORCID,Gallacher Ryan J.¹²,Keir Derek¹³^ORCID,Ebinger Cynthia J.²^ORCID,Mtelela Khalfan⁴

Affiliation:

1. Ocean and Earth Science, National Oceanography Centre Southampton; University of Southampton; Southampton UK

2. Department of Earth and Environmental Sciences; Tulane University of Louisiana; New Orleans LA USA

3. Dipartimento di Scienze della Terra; Università degli Studi di Firenze; Florence Italy

4. Department of Geology; University of Dar es Salaam; Dar es Salaam Tanzania

Funder

NERC Grant

NERC studentship

National Eye Research Centre

Natural Environment Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

Reference79 articles.

3. How much magma is required to rift a continent?;Bialas;Earth and Planetary Science Letters,2010

4. Consequences of asthenospheric variability on continental rifting;Buck;Rheology and deformation of the lithosphere at continental margins,2004

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