| Citation: |
The Invasion of Remote Groundwater into Deserts on the Alxa Plateau: Acid Soluble Sr Isotopic Evidence[J]. Journal of South China Normal University (Natural Science Edition), 2014, 46(3).
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[1]杨小平.巴丹吉林沙漠腹地湖泊的水化学特征及其全新世以来的演变[J].第四纪研究, 2002, 22(2):97-104
[2]Yang X P.Water chemistry of the lakes in the Badain Jaran Desert and their Holocene evolution[J].Quaternary Sciences, 2002, 22(2):97-104 [3]Chen J S, Li L, Wang J Y, et al.Groundwater maintains dune landscape [J]. Nature, 2004, 432-459. [4]Yang X P, Williams M A J.The ion chemistry of lakes and late Holocene desiccation in the Badain Jaran Desert, Inner Mongolia, China [J]. Catena, 2003, 51:45-60. [5]Zhang H C, Ma Y Z, Wünnemann B, et al.A Holocene climatic record from arid northwestern China [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2000, 162: 389-401. [6]Yang B, Shi Y F, Braeuning A, et al.Evidence for a warm-humid climate in arid northwestern China during 40–30 ka BP [J]. Quaternary Science Reviews, 2004, 23: 2537–2548. [7]Miller E K, Blum J D, Friedland A J.Determination of soil exchangeable-cation loss and weathering rates using Sr isotopes [J]. Nature, 1993, 362: 438-441. [8]Rao W B, Chen J, Yang J D, et al.Sr-Nd isotopic characteristics of different particle-size fractions of eolian sands in the deserts of northern China[J].Geological Journal of China Universities, 2009, 15(2):159-164 [9]Zhang J, Takahashi K, Wushiki H, et al.Water geochemistry of the rivers around the Taklimakan Desert (NW China): Crustal weathering and evaporation processes in arid land [J]. Chemical Geology, 1995, 119: 225-237. [10]Yokoo Y, Nakano T, Nishikawa M, et al.The importance of Sr isotopic compositions as an indicator of acid-soluble minerals in arid soils in China [J]. Water, Air, and Soil Pollution, 2001, 130: 763-768. [11]Honda M, Shimizu H.Geochemical, mineralogical and sedimentological studies on the Taklimakan Desert sands [J]. Sedimentology, 1998, 45: 1125-1143. [12]Wang Y Q, Zhang X Y, Arimoto R, et al.Characteristics of carbonate content and carbon and oxygen isotopic composition of northern China soil and dust aerosol and its application to tracing dust sources [J]. Atmospheric Environment, 2005, 39: 2631-2642. [13]Yang J D, Chen J, An Z S, et al.Variations in 87Sr/86Sr ratios of calcites in Chinese loess: a proxy for chemical weathering associated with the East Asian summer monsoon [J]. Palaeogeography, Paleoclimatology, Palaeoecology, 2000, 157: 151-159. [14]Liu C Q, Masuda A, Okada A, et al.Isotope geochemistry of Quaternary deposits from the arid lands in the northern China [J]. Earth and Planetary Science Letters, 1994, 127: 25-38. [15]Yokoo Y, Nakano T, Nishikawa M, et al.Mineralogical variation of Sr–Nd isotopic and elemental compositions in loess and desert sand from the central Loess Plateau in China as a provenance tracer of wet and dry deposition in the northwestern Pacific [J]. Chemical Geology, 2004, 204: 45–62. [16]Nakano T, Yokoo Y, Nishikawa M, et al.Regional Sr-Nd isotopic ratios of soil minerals in northern China as Asian dust fingerprints [J]. Atmospheric Environment, 2004, 38: 3061-3067.
[1]杨小平.巴丹吉林沙漠腹地湖泊的水化学特征及其全新世以来的演变[J].第四纪研究, 2002, 22(2):97-104
[2]Yang X P.Water chemistry of the lakes in the Badain Jaran Desert and their Holocene evolution[J].Quaternary Sciences, 2002, 22(2):97-104 [3]Chen J S, Li L, Wang J Y, et al.Groundwater maintains dune landscape [J]. Nature, 2004, 432-459. [4]Yang X P, Williams M A J.The ion chemistry of lakes and late Holocene desiccation in the Badain Jaran Desert, Inner Mongolia, China [J]. Catena, 2003, 51:45-60. [5]Zhang H C, Ma Y Z, Wünnemann B, et al.A Holocene climatic record from arid northwestern China [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2000, 162: 389-401. [6]Yang B, Shi Y F, Braeuning A, et al.Evidence for a warm-humid climate in arid northwestern China during 40–30 ka BP [J]. Quaternary Science Reviews, 2004, 23: 2537–2548. [7]Miller E K, Blum J D, Friedland A J.Determination of soil exchangeable-cation loss and weathering rates using Sr isotopes [J]. Nature, 1993, 362: 438-441. [8]Rao W B, Chen J, Yang J D, et al.Sr-Nd isotopic characteristics of different particle-size fractions of eolian sands in the deserts of northern China[J].Geological Journal of China Universities, 2009, 15(2):159-164 [9]Zhang J, Takahashi K, Wushiki H, et al.Water geochemistry of the rivers around the Taklimakan Desert (NW China): Crustal weathering and evaporation processes in arid land [J]. Chemical Geology, 1995, 119: 225-237. [10]Yokoo Y, Nakano T, Nishikawa M, et al.The importance of Sr isotopic compositions as an indicator of acid-soluble minerals in arid soils in China [J]. Water, Air, and Soil Pollution, 2001, 130: 763-768. [11]Honda M, Shimizu H.Geochemical, mineralogical and sedimentological studies on the Taklimakan Desert sands [J]. Sedimentology, 1998, 45: 1125-1143. [12]Wang Y Q, Zhang X Y, Arimoto R, et al.Characteristics of carbonate content and carbon and oxygen isotopic composition of northern China soil and dust aerosol and its application to tracing dust sources [J]. Atmospheric Environment, 2005, 39: 2631-2642. [13]Yang J D, Chen J, An Z S, et al.Variations in 87Sr/86Sr ratios of calcites in Chinese loess: a proxy for chemical weathering associated with the East Asian summer monsoon [J]. Palaeogeography, Paleoclimatology, Palaeoecology, 2000, 157: 151-159. [14]Liu C Q, Masuda A, Okada A, et al.Isotope geochemistry of Quaternary deposits from the arid lands in the northern China [J]. Earth and Planetary Science Letters, 1994, 127: 25-38. [15]Yokoo Y, Nakano T, Nishikawa M, et al.Mineralogical variation of Sr–Nd isotopic and elemental compositions in loess and desert sand from the central Loess Plateau in China as a provenance tracer of wet and dry deposition in the northwestern Pacific [J]. Chemical Geology, 2004, 204: 45–62. [16]Nakano T, Yokoo Y, Nishikawa M, et al.Regional Sr-Nd isotopic ratios of soil minerals in northern China as Asian dust fingerprints [J]. Atmospheric Environment, 2004, 38: 3061-3067. |
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