[1] |
(1)Thorez.J.,1976,practical identification of clay minerals, G.L elotte,Ed. Dison,Belgique. (2)MaxwelI,D.T.and Hower, J.,1967,High-grade diagenesis and low-grade metam- orphism of illite in Precambrian Belt,Amer.Min.,52, 843-857。 (3)Weaver,C.E.,1960,Possibld uses of clay minerals in search for oil,Bull. Am.Assoc. Geol.44,I505-1518. (4)Weaver,C.E.,1961,Clay minerals of the O nachita structural belt and adjacent foreland.in:the O nachita system,the U niv. T exeas Publ.,6120,Bureau Econ. Geol.Austin,147-160. (5)Dunoyer de Segonzac,G.,1969,Les mineraux argileux dans la diagenese- passage au metamorphisme,Mem.29,serv Carte Geols. Als Lorr.,320p. (6)Frey,M.,1970,The step from diagenesis to metamophism in pelitic rocks during Alpine Orogenesis,Sedimentology,15,261-279. (7)Post, J.L.,and Plummer,C.C.,1972, T he chlorite series of Flagstaff Hillarea,California:a preliminary investigaton,Clays and Clay Min.,20,271-283. (8)Johns,W.D.,Grim,R.E.and Bradley,W.F.,1954, Quantitative estimations of minerals by diffraction methods, J.Sed.Petrol,24, 242-251. (9)Brindley,G.W. and De Kimpe, C.,1961,Identification of clay minerals by single crystal electron diffraction,T he A m erican mineralogist,46,P1005. (10) Clauer,N.,1979, A ne w approach to Rb-Sr dating of sedimentary rock,In: E.Jager and J.C.Hunziker (Editors),L ectures in Isotope Geology,Springer- Verlag,Berlin, 30-51 (11) Kisck,H.J.,1983,Mineralogy and petrology of burial diagenesis(burial metam-orphism) and incipient metamorphism in elastic rocks,In:G.,Larsen and G.V., Chilingar (Editors),Developments in Sedimentology 25R, Elsevier, 289-494. (12) White,W.A.,1961,Colloidal phenomena in sedimentation of argillaceous rocks, J .sediment.Petrol.,31,560-570. (13) Meade,R.H.,1966,E actors influencing the early stages of the co m paction of claps and sands-review,).Sediment.petrol.,36,1085-1101. |