Contribution of detrital materials from the Yukon River to the continental shelf sediments of the Bering Sea based on the electron spin resonance signal intensity and crystallinity of quartz

Deep-Sea Research Part II: Topical Studies in Oceanography

Volumn 61-64, Issue , 2012, Pages 145-154

  Nagashima, Kana ^a   Asahara, Yoshihiro ^b   Takeuchi, Fumi ^b   Harada, Naomi ^a   Toyoda, Shin ^c   Tada, Ryuji ^d  

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

^b NAGOYA UNIVERSITY   (Japan)

^c OKAYAMA UNIVERSITY OF SCIENCE   (Japan)

^d UNIVERSITY OF TOKYO   (Japan)

Author keywords

Bering Sea; Crystallinity; Electron spin resonance; Provenance; Quartz; Yukon River

Indexed keywords

BERING SEA; CONTINENTAL SHELVES; CORE-TOP SAMPLES; CRYSTALLINITIES; DRAINAGE BASIN; HYDROLOGICAL CYCLES; PROVENANCE; SPATIAL DISTRIBUTION PATTERNS; SPATIAL EXTENT; SPATIAL PATTERNS; STORM SURGES; SUSPENDED MATERIAL; WIDE AREA;

ANOXIC SEDIMENTS; CLIMATE CHANGE; MATERIALS; PARAMAGNETIC RESONANCE; QUARTZ; SILT;

RIVERS;

CONTINENTAL SHELF; CONTINENTAL SLOPE; CRYSTALLINITY; DETRITAL DEPOSIT; DRAINAGE BASIN; ELECTRON SPIN RESONANCE; HYDROLOGICAL CYCLE; MARINE SEDIMENT; MELTING; PALEOCLIMATE; PROVENANCE; QUARTZ; SEDIMENT TRANSPORT; SIGNAL; SPATIAL DISTRIBUTION; STORM SURGE;

ARCTIC; BERING SEA; PACIFIC OCEAN; YUKON RIVER;

EID: 84857445015     PISSN: 09670645     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.dsr2.2011.12.001     Document Type: Article

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