Modification of Graben Along the Dichotomy Boundary in Eastern Arabia Terra (Coloe Fossae; 53-59°E, 37-41°N): Nature and Evolution of Lobate Debris Aprons and Their Relationships to Lineated Valley Fill and Glacial Systems

Details Modification of Graben Along the Dichotomy Boundary in Eastern Arabia Terra (Coloe Fossae; 53-59°E, 37-41°N): Nature and Evolution of Lobate Debris Aprons and Their Relationships to Lineated Valley Fill and Glacial Systems Modification of Graben Along the Dichotomy Boundary in Eastern Arabia Terra (Coloe Fossae; 53-59°E, 37-41°N): Nature and Evolution of Lobate Debris Aprons and Their Relationships to Lineated Valley Fill and Glacial Systems

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1317d&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1317

Physics

1

Scientific paper

Linear lobate debris aprons (LDAs) form in Coloe Fossae, creating
central breached folds; LDA/LVF transitions are common at the dichotomy
boundary, supporting the presence of an integrated Amazonian glacial
landsystem for this area.

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