4常用玄武岩构造环境判别图解.ppt

常用玄武岩构造环境判别图解?主量元素图解?微量元素图解?与残留辉石有关的判别图解参考文献 Pearce J analysis of major element patterns in of Petrol.,1976 (17):15-43. Pearce T. H., Gorman and Birkett . The TiO2-K2O-P2O5 diagram: A method of discriminating between oceanic and non-oceanic basalts. Earth and ary Science Letters. 1975(24):419-426. Pearce T. H., Gorman B. E., Birkett T. C. The relationship between major element chemistry and tectonic environment of basic and intermediate volcanic rocks. Earth and ary Science Letters, 1977(36): 121-132. Mullen E. D. MnO/TiO2/P2O5: a minor element discriminant for basaltic rocks of oceanic environ- ments and its implications for petrogenesis . Earth and ary Science letters, 1983(62): 53-62. Floyd P. A., Winchester J. A. Magma type and tectonic setting discrimination using immobile elements. Earth and ary Science Letters, 1975, (27): 211-218. MacDonald T. K. position of Hawaiian lavas, J. Petrol., 1964(5):82-133. Schwarzer ., Rogers W. A parison of alkali olivine basalts and their differentiation trends, Earth and ary Science Letters, 1974(23):286-296. Holm P. E. Non-recognition of continental tholeiites using the Ti-Y- Zr diagram. Contib . Mineral and Petrol, 1982,(79):308-310. Pearce ., Cann R. Tectonic setting of basic volcanic rocks determined using trace element analyses. Earth and ary Science Letters, 1973 (19):290-300. Prestvik T. Basic volcanic rocks and tectonic setting: A discussion of the Zr -Ti-Y discrimination diagram and its suitability for classification purposes. Lithos , 1982 (15): 241-247. Meschede M. A method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with the Nb-Zr-Y diagram. Chemical Geology, 1986 (56): 207-218. Pearce J. A. and Norry M. J. ic implications of Ti, Zr , Y and Nb variations in volcanic rocks. Contrib. Mineral. Petrol.,1979(69):33- 47. David A. Wood J. L. Joron,Michel Re-appraisal of the use of tr