scholarly article | Q13442814 |
P819 | ADS bibcode | 2013GGG....14.2615S |
P356 | DOI | 10.1002/GGGE.20162 |
P50 | author | Dominik Weiss | Q43172737 |
Youbin Sun | Q47250735 | ||
P2093 | author name string | Min Lin | |
Yan Yan | |||
Ryuji Tada | |||
Hongyun Chen | |||
Shin Toyoda | |||
Yuko Isozaki | |||
P2860 | cites work | Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China | Q34118465 |
Global iron connections between desert dust, ocean biogeochemistry, and climate | Q34407833 | ||
Formation and decay of the E1' center and of its precursor | Q47325279 | ||
Late Pliocene-Pleistocene changes in mass accumulation rates of eolian deposits on the central Chinese Loess Plateau | Q57146274 | ||
Bimodal grain-size distribution of Chinese loess, and its palaeoclimatic implications | Q57146426 | ||
Grain size distribution of quartz isolated from Chinese loess1 paleosol | Q57146787 | ||
Glacial and interglacial patterns for Asian dust transport | Q57146881 | ||
Grain Size of Quartz as an Indicator of Winter Monsoon Strength on the Loess Plateau of Central China during the Last 130,000 Yr | Q57147095 | ||
Atmospheric trace elements over source regions for Chinese dust: concentrations, sources and atmospheric deposition on the Loess plateau | Q57147135 | ||
Geochemistry of the Xining, Xifeng and Jixian sections, Loess Plateau of China: eolian dust provenance and paleosol evolution during the last 140 ka | Q57883342 | ||
Increasing Nd isotopic ratio of Asian dust indicates progressive uplift of the north Tibetan Plateau since the middle Miocene | Q58081485 | ||
Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implications | Q58082522 | ||
Natural and anthropogenic sources of East Asian dust | Q58159924 | ||
The influence on climate forcing of mineral aerosols from disturbed soils | Q59066552 | ||
Seasonal variability in the origin of recent atmospheric mineral dust at NorthGRIP, Greenland | Q59272665 | ||
Lead atmospheric deposition rates and isotopic trends in Asian dust during the last 9.5kyr recorded in an ombrotrophic peat bog on the eastern Qinghai–Tibetan Plateau | Q59906961 | ||
Improved provenance tracing of Asian dust sources using rare earth elements and selected trace elements for palaeomonsoon studies on the eastern Tibetan Plateau | Q59906964 | ||
Millennial-scale oscillations of the westerly jet path during the last glacial period | Q59906967 | ||
Tracing the provenance of fine-grained dust deposited on the central Chinese Loess Plateau | Q59906991 | ||
Contribution of aeolian dust in Japan Sea sediments estimated from ESR signal intensity and crystallinity of quartz | Q59906992 | ||
Distinguishing the sources of Asian dust based on electron spin resonance signal intensity and crystallinity of quartz | Q59906997 | ||
Nd and Sr isotopic characteristics of Chinese deserts: Implications for the provenances of Asian dust | Q59907000 | ||
Provenance of loess material and formation of loess deposits on the Chinese Loess Plateau | Q60142308 | ||
Gustiness: The driver of glacial dustiness? | Q107046718 | ||
P433 | issue | 8 | |
P304 | page(s) | 2615-2627 | |
P577 | publication date | 2013-08-01 | |
P1433 | published in | G3: Geochemistry, Geophysics, Geosystems | Q15759647 |
P1476 | title | ESR signal intensity and crystallinity of quartz from Gobi and sandy deserts in East Asia and implication for tracing Asian dust provenance | |
P478 | volume | 14 |