Berner E K,Berner R A.1996.Global Environment:Water,Air and Geochemical Cycles.Prentice-Hall,Upper Saddle River,NJ,376 pp.
[6]
Galy A,France-Lanord C.2001.Higher erosion rates in the Himalaya:Geochemical constraints on riverine fluxes.Geology,29:23～26.
[7]
Huh Y,Tsoi M Y,Zaitsev A,Edmond J.1998.The fluvial geochemistry of the rivers of Eastern Siberia:Ⅰ.Tributaries of the Lena River draining the sedimentary platform of the Siberian Craton.Geochim.Cosmochim.Acta,62:1657～1676.
[8]
Huh Y,Panteleyev G,Babich D,Zaitsev A,Edmond J M.1998a.The fluvial geochemistry of the rivers of Eastern Siberia:Ⅱ.Tributaries of the Lena,Omoloy,Yana,Indigirka,Kolyma and Anadyr draining the collisional/accretionary zone of the Verkhoyansk and Cherskiy ranges.Geochim.Cosmochim.Acta,62:2053～2075.
[9]
Karim A,Veizer J.2000.Weathering processes in the Indus River Basin:implications from riverine carbon,sulfur,oxygen,and strontium isotopes.Chem.Geol.,170:153～177.
[10]
Krishnaswami S,Trivedi J R,Sarin M M,Ramesh R,Sharma K K.1992.Strontium isotopes and rubidium in the Ganga--Brahmaputra river system:Weathering in the Himalaya,fluxes to the Bay of Bengal and contributions to the evolution of oceanic 87Sr/86Sr.Earth Planet.Sci.Lett.,109:243～253.
[11]
Li Jingying,Zhang Jing.2005.Chemical weathering processes and atmospheric CO2 consumption of Huang He River and Chang Jiang River basins.Chinese Geograph.Sci.,15:16～21.
[12]
Millot R,Gaillardet J,Dupré B,Allègre C J.2003.Northern latitude chemical weathering rates:clues from the Mackenzie River Basin,Canada.Geochim.Cosmochim.Acta,67:1305～1329.
[13]
Palmer M R,Edmond J M.1989.The strontium isotope budget of the modern ocean.Earth Planet.Sci.Lett.,92:11～26.
[14]
Palmer M.R.,Edmond J.M.,1992.Controls over the strontium isotope composition of river water.Geochim.Cosmochim.Acta,56:2099～2111.
[15]
Pande K,Sarin M M,Trivedi J R,Krishnaswami S,Sharma K K.1994.The Indus system (India-Pakistan):Major ion chemistry,uranium and strontium isotopes.Chem.Geol.,116:245～259.
[16]
Probst J L,Mortatti J,Tardy Y.1994.Carbon river fluxes and weathering CO2 consumption in the Congo and Amazon river basins.Appl Geochem.,9:1～13.
[17]
Qin Jianhua,Huh Y,Edmond J M,Gu Du,Ran Jing.2006.Chemical and physical weathering in the Min Jing,a headwater tributary of the Yangtze River.Chem.Geol.,227:53～69.
[18]
Quade J,Roe L,DeCelles P G,Ojha T P.1997.The late Neogene 87Sr/86Sr record of lowland Himalayan rivers.Science,276:1828～1831.
[19]
Raymo M E,Ruddiman W F,Froelich P N.1988.Influence of late Cenozoic mountain-building on ocean geochemical cycles.Geology,16:649～653.
[20]
Raymo M E,Ruddiman W F.1992.Tectonic forcing of late Cenozoic climate.Nature,359:117～122.
[21]
Singh S K,Kumar A,France-Lanord C.2006.Sr and 87Sr/86Sr in waters and sediments of the Brahmaputra river system:Silicate weathering,CO2 consumption and Sr flux.Chem.Geol.,234:308～320.
[22]
Suchet P A,Probst J L.1995.A global model for present-day atmospheric/soil CO2 consumption by chemical erosion of continental rocks (GEM-CO2).Tellus,47B:273～280.
[23]
Wu Lingling,Huh Y,Qin Jianhua,Du Gu,Van Der LEE S.2005.Chemical weathering in the Upper Huang He (Yellow River)draining the eastern Qinghai Plateau.Geochim.Cosmochim.Acta,69:5279～5294.
Berner R A,Lassaga A C,Garrels R M.1983.The carbonatesilicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years.Am.J.Sci.,284:1183～1192.
[26]
Bickle M J,Bunbury J,Chapman H J,Harris N B W,Fairchild I J,Ahmad T.2003.Fluxes of Sr into the headwaters of the Ganges.Geochim.Cosmochim.Acta,67:2567～2584.
[27]
Bickle M J,Chapman H J,Bunbury J,Harris N B W,Fairchild I J,Ahmad T,Pomies C.2005.Relative contributions of silicate and carbonate rocks to riverine Sr fluxes in the headwaters of the Ganges.Geochim.Cosmochim.Acta,69:2221～2240.
[28]
Blum J D,Gazis C A,Jacobson A D,Chamberlain C P.1998.Carbonate versus silicate weathering in the Raikhot watershed within the High Himalayan Crystalline Series.Geology,26:411～414.
[29]
Dalai T K,Krishnaswami S,Sarin M M.2002.Major ion chemistry in the headwaters of the Yamuna river system:Chemical weathering,its temperature dependence and CO2 consumption in the Himalaya.Geochim.Cosmochim.Acta,66:3397～3416.
[30]
Edmond J M.1992.Himalayan tectonics,weathering processes,and the strontium isotope record in marine limestones.Science,258:1594～1597.
[31]
Edmond J M,Palmer J R,Measures C I,Brown E T,Huh Y.1996.Fluvial geochemistry of the eastern slope of the northeastern Andes and its foredeep in the drainage of the Orinoco in Colombia and Venezuela.Geochim.Cosmochim.Acta,60:2949～2976.
[32]
Gaillardet J,Duprè B,Allègre C J.1995.A global geochemical mass budget applied to the Congo Basin rivers:Erosion rates and continental crust composition.Geochim.Cosmochim.Acta,59:3469～3485.
[33]
Gaillardet J,Duprè B,Louvat P,Allègre C J.1999.Global silicate weathering and CO2 consumption rates deduced from the chemistry of large rivers.Chem.Geol.,159:3～30.
[34]
Galy A,France-Lanord C.1999.Weathering processes in the Ganges-Brahmaputra basin and the riverine alkalinity budget.Chem.Geol.,159:31～60.
[35]
Ludwig W,Probst J L,Kempe S.1996.Predicting the oceanic input of organic carbon by continental erosion.Global Biochem Ccycles,10(1):23～41.
[36]
Meybeck M,1987.Global chemical weathering of surficial rocks estimated from river dissolved loads.Am.J.Sci.287:401～428.
[37]
Roy S,Gaillardet J,Allègre C J.1999.Geochemistry of dissolved and suspended loads of the Seine river,France:anthropogenic impact,carbonate and silicate weathering.Geochim.Cosmochim.Acta,63 (9):1277～1292.
[38]
Sarin M M,Krishnaswami S,Dilli K,Somayajulu B L K,Moore W S.1989.Major ion chemistry of the Ganga-Brahmaputra river system:Weathering processes and fluxes to the Bay of Bengal.Geochim.Cosmochim.Acta,53:997～1009.
[39]
Singh S K,Trivedi J R,Pande K,Ramesh R,Krishnaswam,S.1998.Chemical and strontium,oxygen,and carbon isotopic compositions of carbonates from the Lesser Himalaya:Implications to the strontium isotope composition of the source waters of the Ganga,Ghaghara,and the Indus rivers.Geochim.Cosmochim.Acta,62:743～755.
[40]
Singh S K,Sarin M M,France-Lanord C.2005.Chemical erosion in the eastern Himalaya:Major ion composition of the Brahmaputra and 13C of dissolved inorganic carbon.Geochim.Cosmochim.Acta,69:3573～3588.
