Takematus N.Factor regulating the distribution of elements in marine sediments predicted by a simulatiai model.Journal Oceanography,1993,49(4):425-442
[3]
Leinen M.The origin of palaeochemical signature in North Pacific pelagic clays:parting experiments.Geochemica et Cosmchirnica Acto,1987,51(2):305-319
[4]
Ross M R.An algprithmforconstructing extrene corrrpositions.Canputer&Geology,1996,22,15-25
[5]
Full W E,Ehrlich R,Klovan J E.Extended Q model-objective definition of extermal end members in the analysis of mixtures.Mathematical Geology,1981,13,331-344
[6]
Miesch A.T.Q-model factor analysis of composition data.Computer & Geosciences.,1976.1,147-159
[7]
Klovan J E,Miesch A T.Extended CABFAC and Q model-canputer progrms for Q model factor analysis and compositional data.Computer & Geosciences,1976,1,161-178
[8]
赵一阳,鄂明才.中国浅海沉积地球化学.北京:科学出版社,1994,107-200
[9]
Heath G R.Genesis and transfrmation of metalliferous sediments from the Fast Pacific Rise.Geol.Soc.Amber.,Bull.,1997 88 723-733
[10]
Dymorrd J,Lyle M,Firrney B et al.Ferromanganese nodules fxan MNSOP sites,H,S and R-control of mineralogical and chemical canposition by multiple accretionary processes.Geochemica et Cosmochimica Acta,1984,48(5):931-949
[11]
Renner R M,Glasby G P,Manheim F J et al.Partitim process for geochemistry data sets:a geological survey of Canada,1989,391-328
[12]
Remer R M,A constrained least-squares subroutine for adjusting negative estimated elanent concentrations to zero.Canputer and Geosciences,1993,19(9):1351-1360
[13]
Renner R M,Juke S R.End-manber graphics.J.Math.Geology,1992,24(3):287-303
[14]
Mackas D L.Least squares multiple traces analysis of water mass composition.J.G.R.,1987,92(3):2907-2918
[15]
Edmonds H N.A three component mixing model for ridge crest hydrothemral fluid.Earth and Planetary Science Letters,1995,134,53-67
[16]
Clarke Thomas L.An oblique factor analysis solution for the analysis of mixtures.Marhanatical Geology,1978,10(2):225-241
