The Oligocene‐Miocene Guadalope‐Matarranya Fan, Spain, as an Analog for Long‐Lived, Ridge‐Bearing Megafans on Mars-Reference-Cited by-同舟云学术

The Oligocene‐Miocene Guadalope‐Matarranya Fan, Spain, as an Analog for Long‐Lived, Ridge‐Bearing Megafans on Mars

Published:2021-12 Issue:12 Volume:126 Page:
ISSN:2169-9097
Container-title:Journal of Geophysical Research: Planets
language:en
Short-container-title:JGR Planets

Author:

Hayden A. T.¹²^ORCID,Lamb M. P.¹^ORCID,Myrow P. M.³,Mohrig D.⁴^ORCID,Williams R. M. E.⁵^ORCID,Cuevas Martínez J. L.⁶,Cardenas B. T.¹⁴^ORCID,Findlay C. P.⁷⁸^ORCID,Ewing R. C.⁷^ORCID,McElroy B. J.⁹^ORCID

Affiliation:

1. Division of Geological and Planetary Sciences California Institute of Technology Pasadena CA USA

2. Now at California Council on Science and Technology Sacramento CA USA

3. Geology Department Colorado College Colorado Springs CO USA

4. Department of Geological Sciences The University of Texas at Austin Austin TX USA

5. Planetary Science Institute Tucson AZ USA

6. Departament de Dinàmica de la Terra i de l’Oceà Facultat de Ciències de la Terra Universitat de Barcelona Barcelona Spain

7. Department of Geology and Geophysics Texas A&M University College Station TX USA

8. Now at Chevron Corporation Houston TX USA

9. Department of Geology and Geophysics University of Wyoming Laramie WY USA

Funder

National Aeronautics and Space Administration

Ministerio de Economía, Industria y Competitividad, Gobierno de España

Generalitat de Catalunya

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JE006993

Reference105 articles.

1. Hypotheses for the origin of the Hypanis fan‐shaped deposit at the edge of the Chryse Escarpment, Mars: Is it a Delta?;Adler J. B.;Icarus,2018

2. THE CLASSIFICATION OF CROSS-STRATIFIED UNITS. WITH NOTES ON THEIR ORIGIN

3. A REVIEW OF THE ORIGIN AND CHARACTERISTICS OF RECENT ALLUVIAL SEDIMENTS

4. Variations in fluvial style on the Eocene–Oligocene alluvial fan of the Scala Dei Group, SE Ebro Basin, Spain

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