Reference64 articles.
1. Anderson, A.T. (1967) ‘The dimensions of oxygen isotope equilibrium attainment during prograde metamorphism.’ J. Geol.
75, 323–332.
2. Baker, A.J. (1988) ‘Stable isotopic evidence for limited fluid infiltration of deep crustal rocks from the Ivrea Zone, Italy.’ Geology 16, 492–495.
3. Baker, A.J. ‘Stable isotopic evidence for fluid rock interactions during high grade metamorphism in the Ivrea Zone, Italy.’ Submitted to Journal of Petrology.
4. Baker, A.J. & Fallick, A.E. (1988) ‘Evidence for CO2 infiltration in granulite facies marbles from Lofoten-Vesteralen, Norway’ Earth Planet. Sci. Lett
91, 132–140.
5. Brace, W.F. (1971) ‘Resistivity of saturated crustal rocks to 40 km based on laboratory measurements.’ In Heacock, J.G. (ed.) Structure and physical properties of the earths crust. Geophys. Monogr. Ser. 14, 243–255, AGU, Washington, D.C.
Cited by
4 articles.
订阅此论文施引文献
订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献