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Record ID harvard_bibliographic_metadata/ab.bib.14.20150123.full.mrc:212626012:2387
Source harvard_bibliographic_metadata
Download Link /show-records/harvard_bibliographic_metadata/ab.bib.14.20150123.full.mrc:212626012:2387?format=raw

LEADER: 02387nam a22004215a 4500
001 014157417-8
005 20141003185836.0
008 100715s2009 gw | o ||0| 0|eng d
020 $a9783642036088
020 $a9783642036071 (ebk.)
020 $a9783642036088
020 $a9783642036071
024 7 $a10.1007/978-3-642-03608-8$2doi
035 $a(Springer)9783642036088
040 $aSpringer
050 4 $aQE1-996.5
072 7 $aRBG$2bicssc
072 7 $aSCI031000$2bisacsh
082 04 $a551$223
100 1 $aTrouw, Rudolph A. J.,$eauthor.
245 10 $aAtlas of Mylonites- and related microstructures /$cby Rudolph A. J. Trouw, Cees W. Passchier, Dirk J. Wiersma.
264 1 $aBerlin, Heidelberg :$bSpringer Berlin Heidelberg :$bSpringer,$c2009.
300 $aVIII, 322p. 486 illus., 472 illus. in color.$bonline resource.
336 $atext$btxt$2rdacontent
337 $acomputer$bc$2rdamedia
338 $aonline resource$bcr$2rdacarrier
347 $atext file$bPDF$2rda
505 0 $aCataclasites -- Pseudotachylytes -- Low-Grade Mylonites -- Medium-Grade Mylonites -- High-Grade Mylonites -- Protomylonite, Mylonite and Ultramylonite -- Mylonites Derived From Parent Rocks Other Than Granites and Gneisses -- Shear Sense Indicators -- Crystal-Plastic Deformation, Recovery and Recrystallisation of Quartz -- “False” mylonites -- Exercises.
520 $aMylonites form in response to high rates of strain within deep ductile shear zones, which are the extensions at depth of surface faults, thrusts and fault breccias. They can have many different mineralogical compositions and are therefore defined by their textural appearance. This atlas provides high definition images of a large number of different mylonites allowing students and geologists to correctly classify them with greater ease. It also offers insights into the interpretation of mylonitic fabrics to answer questions such as: from what type of rock did this mylonite derive? what were the metamorphic circumstances during mylonitization? what was the intensity of deformation? and what was the sense of shear?
650 20 $aGeology.
650 10 $aEarth sciences.
650 0 $aGeography.
650 0 $aGeology.
700 1 $aWiersma, Dirk J.,$eauthor.
700 1 $aPasschier, Cees W.,$eauthor.
776 08 $iPrinted edition:$z9783642036071
988 $a20140910
906 $0VEN