Ultrahigh-Pressure Metamorphism : 25 Years After The Discovery Of Coesite And Diamond.
- نوع فایل : کتاب
- زبان : انگلیسی
- مؤلف : Larissa Dobrzhinetskaya; International Lithosphere Program.; et al
- ناشر : Burlington : Elsevier Science
- چاپ و سال / کشور: 2011
- شابک / ISBN : 9780123851444
Description
Frontiers of ultrahigh-pressure metamorphism: view from field and laboratory / Larissa F. Dobrzhinetskaya and Shah Wali Faryad -- Part I. Diamonds--new studies -- Diamond--lonsdaleite--graphite relations examined by Raman mapping of carbon microinclusions inside zircon at Kumdy Kol, Kokchetav, Kazakhstan: evidence of the metamictization of diamond / David C. Smith ... [et al.] -- Diamond and other possible ultradeep evidence discovered in the orogenic spinel-garnet peridotite from the Moldanubian zone of the Bohemian Massif, Czech Republic / Kosuke Naemura ... [et al.] -- Diamond formation from amorphous carbon and graphite in the presence of COH fluids: an in situ high-pressure and -temperature laser-heated diamond anvil cell experimental study / Junfeng Zhang ... [et al.] -- Origin of high-pressure disordered metastable phases (lonsdaleite and incipiently amorphized quartz) in metamorphic rocks: geodynamic shock or crystal-scale overpressure? / Gaston Godard ... [et al.] -- Part II. Minerals chemistry, reactions, and microstructures in UHPM rocks -- Origin and metamorphic evolution of garnet clinopyroxenite from the Sulu UHP terrane, China: evidence from mineral chemisty and microstructures / Ru Y. Zhang ... [et al.] -- The correlation between Raman spectra and the mineral composition of muscovite and phengite / Huijuan Li, Lifei Zhang, and Andrew G. Christy -- Increasing chlorinity in fluids among the prograde metamorphic path: evidence of apatite from Yangkou Eclogite, Sulu, China / Jingbo Liu ... [et al.] -- Trace element and O-isotope composition of polyphase metamorphic veins of the Ile de Groix (Armorican Massif, France): implication for fluid flow during HP subduction and exhumation processes / Afifé El Korh ... [et al.] -- Part III. Geochronological data of UHPM terranes -- Geochronology of the alpine UHP Rhodope zone: a review of isotopic ages and constraints on the geodynamic evolution / Anthi Liati, Dieter Gebauer, and C. Mark Fanning -- Coherence of the Dabie Shan UHPM terrane investigated by Lu-Hf and ⁴⁰Ar/³⁹Ar dating of eclogites / Fraukje M. Brouwer ... [et al.] -- Part IV. Ultrahigh-pressure metamorphic belts and protolith history of eclogite and garnet peridotite -- Distribution and geological position of high-/ultrahigh-pressure units within the European Variscan Belt: a review / Shah Wali Faryad -- Ultramafic cumulates of oceanic affinity in an intracontinental subduction zone: ultrahigh-pressure garnet peridotites from Pohorje (Eastern Alps, Slovenia) / Jan C.M. De Hoog ... [et al.] -- Very high pressure epidote eclogite from Ross River area, Yukon, Canada, records deep subduction / Edward Ghent and Philippe Erdmer -- HP-UHP metamorphic belts in the eastern Tethyan orogenic system in China / Jingsui Yang ... [et al.] -- Orogenic garnet peridotites: tools to reconstruct paleo-geodynamic settings of fossil continental collision zones / Cong Zhang, Herman van Roermund, and Lifei Zhang -- Petrology, geochemistry, geochronology, and metamorphic evolution of garnet peridotites from south Altyn Tagh UHP terrane, northwestern China: records related to crustal slab subduction and exhumation history / Chao Wang ... [et al.] -- Metamorphic evolution of the Gridino mafic dyke swarm (Belomorian Eclogite province, Russia) / Ksenia A. Dokukina and Alexander N. Konilov -- The Salma eclogites of the Belomorian province, Russia: HP/UHP metamorphism through the subduction of mesoarchean oceanic crust / Alexander N. Konilov ... [et al.].
Ultrahigh pressure metamorphism (UHPM) is a relatively new but fast growing discipline related to the deep subduction of slabs of continental and/or oceanic crust into the Earth's mantle and their return towards the surface as important components of mountain belts. The discipline was established ~25 years ago after discoveries of high pressure minerals, coesite and diamond, in the rocks of the continental affinities, a place where such minerals are "forbiden"according to main geological concepts. Exposures of HP/UHP rocks, once thought to be restricted to European Mountain systems, are being.