Where fast weathering creates thin regolith and slow weathering creates thick regolith

Earth Surface Processes and Landforms

Volumn 38, Issue 8, 2013, Pages 847-858

  Bazilevskaya, Ekaterina ^a   Lebedeva, Marina ^a   Pavich, Milan ^b   Rother, Gernot ^c   Parkinson, Dilworth Y ^d   Cole, David ^e   Brantley, Susan L ^a  

^a PENNSYLVANIA STATE UNIVERSITY   (United States)

^b U S GEOLOGICAL SURVEY   (United States)

^c OAK RIDGE NATIONAL LABORATORY   (United States)

^d LAWRENCE BERKELEY NATIONAL LABORATORY   (United States)

^e OHIO STATE UNIVERSITY   (United States)

Author keywords

Fluid transport; Geomorphology; Nanoporosity; Neutron scattering; Regolith thickness

Indexed keywords

FELDSPAR; FLOW OF FLUIDS; GEOMORPHOLOGY; GRANITE; MICA; NEUTRON SCATTERING; POROSITY; TRANSPORT PROPERTIES;

DEEP OXIDATION; EARTH MATERIALS; FLUID TRANSPORT; LAND SURFACE; MICROFRACTURES; NANOPOROSITY; REGOLITH THICKNESS; ROCK COMPOSITION;

WEATHERING;

DIABASE; FLUID FLOW; GEOMORPHOLOGICAL RESPONSE; GRANITE; HYDROLOGICAL RESPONSE; NEUTRON SCATTERING; OBSERVATIONAL METHOD; PORE SPACE; POROSITY; REGOLITH; WEATHERING PROFILE; WEATHERING RATE;

UNITED STATES; VIRGINIA;

EID: 84879201764     PISSN: 01979337     EISSN: 10969837     Source Type: Journal    
DOI: 10.1002/esp.3369     Document Type: Article

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