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E-raamat: Rare Earth Elements in Ultramafic and Mafic Rocks and their Minerals: Main types of rocks. Rock-forming minerals [Taylor & Francis e-raamat]

(Institute of Geology and Mineralogy, Novosibirsk, Russia)
  • Formaat: 608 pages, 152 Tables, black and white; 179 Line drawings, black and white; 1 Halftones, black and white
  • Ilmumisaeg: 28-Sep-2010
  • Kirjastus: CRC Press
  • ISBN-13: 9780429213045
Teised raamatud teemal:
  • Taylor & Francis e-raamat
  • Hind: 240,04 €*
  • * hind, mis tagab piiramatu üheaegsete kasutajate arvuga ligipääsu piiramatuks ajaks
  • Tavahind: 342,91 €
  • Säästad 30%
  • Formaat: 608 pages, 152 Tables, black and white; 179 Line drawings, black and white; 1 Halftones, black and white
  • Ilmumisaeg: 28-Sep-2010
  • Kirjastus: CRC Press
  • ISBN-13: 9780429213045
Teised raamatud teemal:
This book gives an overview of the world's literature on analytical data and theoretical concepts of the regularities of rare earth elements (REE) in ultramatic and mafic rocks of different chemcial and mineral compositions - mantle restites (including those composing mantle xenoliths in alkali basaltoids), highly magnesium hypabyssal rocks, plutonic rocks of mafic-ultramafic and ultramafic-mafic massifs, as well as in the main minerals composing these rocks - olivines, orthopyroxenes, clinopyroxenes, plagioclases, and amphiboles. Much attention is given to a comparative analysis of the REE distribution in rocks and minerals from different types of massifs, complexes, and provinces. Various aspects of their intragranular and intermineral distribution are considered, and data on the coefficients of their parlition between minerals and their parental melts as well as between coexisting minerals are generalized. Probable schemes of REE isomorphism in rock-forming minerals are discussed. The generalization is based on the results of analyses of several thousands of rock samples and more than 2000 analyses of minerals, part of which was carried out with samples from author's collections. The book is intended for specialists in petrology and geochemistry of ultramafic, mafic, and other types of igneous rocks as well as students of geological departments of colleges and post-graduate students.
Introduction to the English Edition xi
Preface xiii
Acknowledgments xiv
From the editors xv
Introduction xviii
1 Rare earth elements in ultramafic rocks from mafic-ultramafic massifs of folded regions
1(68)
1.1 Dunites
2(10)
1.2 Harzburgites
12(19)
1.3 Lherzolites
31(19)
1.4 Wehrlites
50(6)
1.5 Clinopyroxenites
56(4)
1.6 Websterites
60(6)
1.7 Summary
66(3)
2 Rare earth elements in ultramafites from deep xenoliths in alkali basalts
69(34)
3 Rare earth elements in hypabyssal and subvolcanic rocks with high in magnesium composition
103(104)
3.1 Kimberlites
103(53)
3.1.1 A brief history of research on the geochemistry of REE in kimberlites
104(3)
3.1.2 Comparative characteristics of the REE composition of kimberlites from major provinces
107(38)
3.1.3 Correlation of REE and other components in kimberlites
145(7)
3.1.4 General regularities of REE distribution in kimberlites
152(4)
3.2 Komatiites
156(21)
3.3 Meimechites
177(2)
3.4 Picrites
179(11)
3.5 Lamproites
190(14)
3.6 Summary
204(3)
4 Rare earth elements in plutonic mafic rocks
207(62)
4.1 Gabbros
208(18)
4.2 Gabbro-norites
226(1)
4.3 Norites
227(7)
4.4 Olivine gabbros
234(12)
4.5 Troctolites
246(5)
4.6 Anorthosites
251(3)
4.7 Eclogites
254(13)
4.8 Summary
267(2)
5 Rare earth elements in rock-forming minerals from ultramafic and mafic rocks
269(244)
5.1 Olivines
269(22)
5.1.1 REE composition of olivines
270(18)
5.1.2 Coefficients of REE distribution between olivines and coexisting phases
288(3)
5.2 Orthopyroxenes
291(30)
5.2.1 REE composition of orthopyroxenes
292(21)
5.2.2 On the relationship between the REE composition and content of fluid components in orthopyroxenes
313(3)
5.2.3 Coefficients of REE distribution between orthopyroxenes and coexisting phases
316(4)
5.2.4 Isomorphism of REE in orthopyroxenes
320(1)
5.3 Clinopyroxenes
321(106)
5.3.1 REE composition of clinopyroxenes
322(78)
5.3.2 Coefficients of REE distribution between clinopyroxenes and coexisting phases
400(19)
5.3.3 Isomorphism of REE in clinopyroxenes
419(8)
5.4 Plagioclases
427(57)
5.4.1 REE composition of plagioclases
428(21)
5.4.2 Experience of systematization of plagioclases on the basis of some parameters of REE distribution
449(16)
5.4.3 Coefficients of REE distribution between plagioclases and coexisting phases
465(11)
5.4.4 Isomorphism of REE in plagioclases
476(2)
5.4.5 Examples of numerical experiments on modeling of the REE composition of parental melts based on data on plagioclases
478(6)
5.5 Amphiboles
484(29)
5.5.1 REE composition of amphiboles
484(8)
5.5.2 Experience of systematization of amphiboles on the basis of some parameters of REE distribution
492(6)
5.5.3 Coefficients of REE distribution between amphiboles and coexisting phases
498(10)
5.5.4 Isomorphism of REE in amphiboles
508(5)
6 Indicator properties of rare earth elements and their role in studies of genesis of rocks and minerals from mafic-ultramafic complexes
513(20)
6.1 REE as indicators of formation and transformation conditions of ultramafic rocks
513(9)
6.2 REE as indicators of formation and transformation conditions of mafic rocks
522(5)
6.3 Indicator properties of REE in study of the formation and transformation of rock-forming minerals of ultramafic and mafic rocks
527(6)
Afterword 533(4)
References 537(24)
Subject index 561(12)
Author index 573
Professor Felix Lesnov graduated at the Geology Department, University of Lviv, Ukraine in 1957. Between 1957 and 1963 he was employed by the USSR Ministry of Geology (field geologist), Ulan-Ude. As of 1963 he is affiliated with the Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences (Novosibirsk). He published more than 250 papers and 8 monographs, dedicated to geology, petrology, petrochemistry , mineralogy, geochemistry, and metallogeny of mafic-ultramafic associations of Chukotka, Kamchatka, Sakhalin Island, Transbaykalia, Mongolia, Urasl, Tian-Shan, Northern Pamir, and other regions.