Last edited by Jujas
Tuesday, July 14, 2020 | History

4 edition of Metamorphic pressure-temperature-time paths found in the catalog.

Metamorphic pressure-temperature-time paths

by Frank S. Spear

  • 379 Want to read
  • 22 Currently reading

Published by American Geophysical Union in Washington, D.C .
Written in English

    Subjects:
  • Metamorphism (Geology),
  • Rock pressure.,
  • Earth temperature.

  • Edition Notes

    StatementFrank S. Spear and Simon M. Peacock.
    SeriesShort course in geology ;, v. 7
    ContributionsPeacock, Simon Muir, 1960-, International Geological Congress (28th : 1989 : Washington, D.C.)
    Classifications
    LC ClassificationsQE475.A2 S68 1989
    The Physical Object
    Paginationviii, 102 p. :
    Number of Pages102
    ID Numbers
    Open LibraryOL2195383M
    ISBN 100875907040
    LC Control Number89014892

    Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths is a monograph on metamorphic petrology written by Frank S. Spear and published by the Mineralogical Society of America. The book introduces concepts at an introductory level, and provides development to a graduate student level, so that the book may be used (selectively) in a variety of courses. Pressure‐temperature‐time paths and the relationship between collision, deformation and metamorphism in the north‐west Himalaya The P‐T‐t paths, derived from inclusion assemblages and forward modelling of garnet zonation patterns, show that this metamorphism was along a path of increasing pressure. Geochronological data date Cited by:

    Metamorphic dehydration reactions that consume 50 kJ/kg result in P‐T‐t paths that are only 5 K cooler than models that neglect such reactions. In both the temperature and amphibole dehydration models, the fluid production region moves to greater depths over time as the subduction zone cools. In book: Encyclopedia of Geology, pp P-T-t paths in dynamothermal metamorphic rocks discussed for these two sequences of mineralogical zonation. Pressure-temperature-time paths.

    In metamorphic rock: Pressure-temperature-time paths Interaction between metamorphic petrologists and geophysicists in the s led to the realization that each metamorphic rock follows its own unique path through pressure- (depth-) temperature space during metamorphism and that these paths bear little or no resemblance to steady-state geotherms.   Citation: Spear, Frank S. Metamorphic Phase Equilibria and Pressure-temperature-time Paths. Washington D.C.: Mineralogical Society of America, Print. ISBN: I couldn't find a digital version of the book anywhere, I'm hoping a scan might exist somewhere.


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Metamorphic pressure-temperature-time paths by Frank S. Spear Download PDF EPUB FB2

Buy Metamorphic Pressure - Temperature - Time Paths (Short Courses in Geology) on FREE SHIPPING on qualified orders Metamorphic Pressure - Temperature - Time Paths (Short Courses in Geology): Spear, Frank S., Peacock, Simon M.: : Books.

Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths,MSA, Monograph Series, pages with illustrations.

Hardcover – by F. Spear (Author)Author: F. Spear. A renaissance in the study of metamorphic rocks has occurred in the past decade. For a long time (with some notable exceptions) metamorphic rocks were studied as examples of heterogeneous systems at equilibrium and the study of metamorphism was, in effect, a phase equilibria experiment.

Additional Physical Format: Online version: Spear, Frank S. Metamorphic pressure-temperature-time paths. Washington, D.C.: American Geophysical Union, © Genre/Form: Electronic books: Additional Physical Format: Print version: Spear, Frank S.

Metamorphic pressure-temperature-time paths. Washington, D.C.: American. (reprinted ) pages. ISBN Now in its second printing, Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths is a monograph on metamorphic petrology written by Frank S.

Spear and published by the Mineralogical Society of America. A companion paper (England & Thompson, a) investigates the pressure-temperature-time (PTt) paths followed by rocks undergoing burial metamorphism in continental thickening events.

This paper discusses problems involved in inferring such paths from the petrological data available in metamorphic rocks and—once such paths are determined—how they may be Cited by:   Calling it a greenschist facies rock tells us about a single point on its journey, but not the whole picture.

Being romantic souls, geologists often refer to this journey as the rock’s Pressure-Temperature-time path, or P-T-t path. Pressure and temperature are the things we can measure, because we understand how they affect metamorphic reactions.

Metamorphic rock - Metamorphic rock - Pressure-temperature-time paths: Interaction between metamorphic petrologists and geophysicists in the s led to the realization that each metamorphic rock follows its own unique path through pressure- (depth-) temperature space during metamorphism and that these paths bear little or no resemblance to steady-state geotherms.

- Buy Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths (Monograph (Mineralogical Society of America).) book online at best prices in India on Read Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths (Monograph (Mineralogical Society of America).) book reviews & author details and more at Free delivery on qualified 5/5(1).

Metamorphic Phase Equilibria And Pressure Temperature Time Paths book. Read 3 reviews from the world's largest community for readers/5. Metamorphic Phase Equilibria And Pressure-Temperature-Time-Paths. Frank S. Spear (reprinted ) pages.

ISBN Now in its second printing, Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths is a monograph on metamorphic petrology written by Frank S. Spear and published by the Mineralogical Society of America. PRESSURE-TEMPERATURE-TIME PATHS FROM ACROSS THE EXHUMED HIMALAYAN METAMORPHIC CORE AND THEIR IMPLICATIONS FOR OROGENIC PROCESSES by Sudip ShresthaTribhuvan University, A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY In THE COLLEGE OF Author: Sudip Shrestha.

Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths,Mineralogical Society of America, MSA, Monograph Series, pages with illustrations.

Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths Mineralogical Society of America Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths Mineralogical Society of America Droop, G. BOOK REVIEWS pattern in the form of scale-invariant geometry in Geoscience, or any other field for that matter.

Petrologic Determination of Metamorphic Pressure‐Temperature‐Time Paths Frank S. Spear Department of Geology, Rensselaer Polytechnic Institute, Troy, New York Cited by: Stanford Libraries' official online search tool for books, media, journals, databases, government documents and more.

Metamorphic phase equilibria and pressure-temperature-time paths in SearchWorks catalog. Metamorphic phase equilibria and pressure-temperature-time paths Mineralogical Society of America short course notes Volume 1 of Monograph (Mineralogical Society of America) Monograph / Mineralogical Society of America Metamorphic Phase Equilibria and Pressure-temperature-time Paths, Mineralogical Society of America: Author: Frank S.

Spear: Editor. pressure-temperature-time (PTt) path followed by a rock during regional metamorphism; more specifically, we concentrate on the PTt paths resulting from the burial and exhumation of rocks during episodes of continental thickening.

UournaJ of Petrotojy. Pin 4, pp.] at Universite Claude Bernard (Lyon 1) on Ma The Pressure-Temperature-time path (P-T-t path) is a record of the pressure and temperature (P-T) conditions that a rock experienced in a metamorphic cycle from burial and heating to uplift and exhumation to the surface.

Metamorphism is a dynamic process which involves the. Pressure-Temperature-Time Paths of Regional Metamorphism II. Their Inference and Interpretation using Mineral Assemblages in Metamorphic Rocks by ALAN BRUCE THOMPSON1 AND PHILIP C.

ENGLAND2 lInstitut fur Mineralogie und Petrographie, ETH Zurich, CH Zurich, Switzerland and ''•Department of Geological Sciences, Harvard University, Cambridge, MA File Size: 2MB. Metamorphism is a dynamic process, involving changes in temperature ± pressure through time. The pressure (P) - temperature (T) - time (t) path of a metamorphic rock is the set of all P-T conditions experienced by a rock during its metamorphic history (Figure 1).

Figure 1. A common pressure-temperature path for regional metamorphism. Spear FS, Peacock SM () Metamorphic pressure-temperature-time paths. American Geophysical Union, Washington CrossRef Google Scholar Spear FS, Hickmott DD, Selverstone J () Metamorphic consequences of thrust emplacement, Fall Author: Vladimir V.

Reverdatto, Igor I. Likhanov, Oleg P. Polyansky, Valentin S. Sheplev, Vasiliy Yu. Kolobo.