2Nicholas C W.Geologically-constrained ubc-gif gravity andmagnetic inversions with examples from the Agnew-Wiluna green-stone belt,Western Australia[]..2008
二级参考文献38
1[1]Backus G E,Gilbert F. Numerical application of a formalism for geophysical inverse problems[J]. Geophys J Roy Astr Soc, 1967,13:247-276.
2[2]Backus G E,Gilbert F. The resolving power of gross earth data[J]. GeophysJ Roy AstrSoc, 1968,16:169-205.
3[3]Parker R L. Best bounds on density and depth from gavity data[J].Geophysics, 1974,39:644-649.
4[4]Parker R L. The theory of ideal bodies for gravity interpreta tion[J]. Geophys J Roy Astr Soc, 1975,42:315-334.
5[5]Huestis S P, Parker R L. Bounding the thickness of oceanic magnetized layer[J]. J Geophys Res, 1977,82:5293-5303.
6[6]Ander M E, Huestis S P. Gravity ideal bodies[J]. Geophysics, 1987,52: 1265- 1278.
7[7]Hoed A E,Kennard R W. Ridge regression: Biased estimation for nonorthogonal problems[J]. Technometrics, 1970,12: 55 -67.
8[8]Lanczos C. Linear differential operators[R]. D Van Nostrand Co,1961.
9[9]Medeiros W E,Silva J B C,Loures L G C L. Symmetric and di rectionally smooth gravity inversion[A]. 62nd Annual Interna tional Meeting[C]. Tulsa:SEG, 1992,529-532.
10[10]Li Y,Oldenburg D W. 3-D inversion of magnetic data[J]. Geophysics, 1996,61:394-408.