South Asian monsoon variability during the past 800 kyr revealed by rock magnetic proxies

Quaternary Science Reviews

Volumn 28, Issue 9-10, 2009, Pages 926-938

  Suganuma, Y ^a,b   Yamazaki, T ^b   Kanamatsu, T ^c  

^a UNIVERSITY OF TOKYO   (Japan)

^b NATIONAL INSTITUTE OF ADVANCED INDUSTRIAL SCIENCE AND TECHNOLOGY AIST   (Japan)

^c JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

CATCHMENTS; GLACIAL GEOLOGY; LITHOLOGY; MAGNETIC FIELDS; MAGNETITE; OCEAN ENGINEERING; OCEANOGRAPHY; OXIDE MINERALS; SEDIMENTARY ROCKS; SWITCHING CIRCUITS;

ASIAN MONSOONS; ASIAN SUMMER MONSOONS; BRAHMAPUTRA RIVERS; CLIMATIC EVENTS; CONTINUOUS SEDIMENTATIONS; EARTH'S MAGNETIC FIELDS; EQUATORIAL INDIAN OCEANS; GEOSYSTEMS; GLACIAL MAXIMUM; GLOBAL CHANGES; GRAIN SIZES; INTENSITY VARIATIONS; MAGHEMITE; MAGNETIC CONCENTRATIONS; MAGNETIC PROXIES; MARINE ISOTOPE STAGES; MID-LATITUDES; PALEOCLIMATIC RECONSTRUCTION; PALEOINTENSITY; PISTON CORES; SILTY CLAYS; TEMPORAL VARIATIONS; TEPHRA LAYERS; WATER DEPTHS;

CLAY MINERALS;

CORE ANALYSIS; INTERGLACIAL; MAGNETIC PROPERTY; MODELING; MONSOON; PEDOGENESIS; RECONSTRUCTION; ROCK PROPERTY; SEASONAL VARIATION; SEDIMENTATION; SYNCHRONY;

INDIAN OCEAN;

EID: 62749139479     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2008.12.014     Document Type: Article

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