Cenozoic Stages of Forearc Evolution Following the Accretion of a Sliver From the Late Cretaceous‐Caribbean Large Igneous Province: SW Ecuador‐NW Peru-Reference-Cited by-同舟云学术

Cenozoic Stages of Forearc Evolution Following the Accretion of a Sliver From the Late Cretaceous‐Caribbean Large Igneous Province: SW Ecuador‐NW Peru

Published:2019-04 Issue:4 Volume:38 Page:1441-1465
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Aizprua Carlos¹²³^ORCID,Witt Cesar²,Johansen Ståle E.¹,Barba Diego⁴^ORCID

Affiliation:

1. Department of Geoscience and PetroleumNorwegian University of Science and Technology (NTNU) Trondheim Norway

2. Laboratoire d'Océanologie et de GéosciencesUniversité de Lille, CNRS, Université du Littoral Côte d'Opale, UMR 8187, LOG Lille France

3. Now at Equinor ASA Bergen Norway

4. Petroamazonas EP Quito Ecuador

Funder

STATOIl AKADEMIA Agreement

Statoil's AKADEMIA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC005235

Reference73 articles.

1. Aizprua C. Witt C. Bronner M. Barba D. &Johansen S. E.(2017).Forearc basin structuring and seismicity patterns controlled by a trapped sliver from the Caribbean large igneous province (CLIP): Northern Andes. Paper presented at William Smith meeting 2017; Plate Tectonics at 50 abstract book Geological Society of London London UK.

2. Aizprua C. Witt C. Johansen S. &Barba D.(2019).Replication Data for: Cenozoic stages of forearc evolution following the accretion of a sliver from the Late Cretaceous‐Caribbean large igneous province (CLIP): SW Ecuador‐NW Peru edited by S. Norwegian University of and Technology DataverseNO.

3. Partitioning of oblique convergence in the Northern Andes subduction zone: Migration history and the present-day boundary of the North Andean Sliver in Ecuador

4. Rapid vertical motions and formation of volcanic arc gaps: Plateau collision recorded in the forearc geological evolution (Costa Rica margin)

5. Regional S-type granites in the Ecuadorian Andes: Possible remnants of the breakup of western Gondwana

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