This book examines the geological aspects of the ultrahigh pressure minerals - diamond and coesite - in the Earth's crust.Hinweis: Dieser Artikel kann nur an eine deutsche Lieferadresse ausgeliefert werden.
1. Overview of the geology and tectonics of UHPM; 2. Experimental and petrogenetic study of UHPM; 3. Principal mineralogical indicators of ultrahigh pressure in crustal rocks; 4. Structures in ultrahigh pressure metamorphic rocks: a case study from the Alps; 5. Creation, preservation, and exhumation of ultrahigh pressure metamorphic rocks; 6. The role of serpentinite melanges in the unroofing of ultrahigh pressure metamorphic rocks: An example from the Western Alps of Italy; 7. Ultrahigh pressure metamorphic rocks in Western Alps; 8. High and ultrahigh pressure eclogites and garnet peridotites in the Scandinavian Caledonides; 9. Microcoesites and microdiamonds in Norway: a brief review; 10. Ultrahigh pressure metamorphic terrane in Eastern Central China; 11. A model for the tectonic history of the high and ultrahigh pressure metamorphic region in East Central China; 12. Diamond-bearing metamorphic rocks of the Kokchetav Massif; 13. Orogenic ultramafic rocks of ultrahigh pressure (diamond facies) origin.
1. Overview of the geology and tectonics of UHPM; 2. Experimental and petrogenetic study of UHPM; 3. Principal mineralogical indicators of ultrahigh pressure in crustal rocks; 4. Structures in ultrahigh pressure metamorphic rocks: a case study from the Alps; 5. Creation, preservation, and exhumation of ultrahigh pressure metamorphic rocks; 6. The role of serpentinite melanges in the unroofing of ultrahigh pressure metamorphic rocks: An example from the Western Alps of Italy; 7. Ultrahigh pressure metamorphic rocks in Western Alps; 8. High and ultrahigh pressure eclogites and garnet peridotites in the Scandinavian Caledonides; 9. Microcoesites and microdiamonds in Norway: a brief review; 10. Ultrahigh pressure metamorphic terrane in Eastern Central China; 11. A model for the tectonic history of the high and ultrahigh pressure metamorphic region in East Central China; 12. Diamond-bearing metamorphic rocks of the Kokchetav Massif; 13. Orogenic ultramafic rocks of ultrahigh pressure (diamond facies) origin.
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