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MARC Record from Library of Congress

Record ID marc_loc_2016/BooksAll.2016.part37.utf8:107130702:2879
Source Library of Congress
Download Link /show-records/marc_loc_2016/BooksAll.2016.part37.utf8:107130702:2879?format=raw

LEADER: 02879cam a22004217i 4500
001 2009939942
003 DLC
005 20140203111753.0
008 091023t20102010gw a qb 000 0 eng d
010 $a 2009939942
020 $a9783642036071 (alk. paper)
020 $a3642036074 (alk. paper)
020 $z9783642036088 (e-ISBN)
035 $a(OCoLC)ocn428028953
040 $aBTCTA$beng$cBTCTA$erda$dYDXCP$dOIP$dOHX$dMUU$dGYG$dOCLCQ$dDLC
042 $alccopycat
050 00 $aQE475.M95$bT76 2010
100 1 $aTrouw, R. A. J.$q(Rudolph A. J.),$d1944-$eauthor.
245 10 $aAtlas of mylonites - and related microstructures /$cRudolph A.J. Trouw, Cees W. Passchier, Dirk J. Wiersma.
264 1 $aHeidelberg ;$aNew York :$bSpringer,$c[2010]
264 4 $c©2010
300 $a322 pages :$bcolor illustrations ;$c29 cm
300 $a1 CD-ROM ;$c4 3/4 in.
336 $atext$btxt$2rdacontent$3text
336 $astill image$bsti$2rdacontent$3CD-ROM
337 $aunmediated$bn$2rdamedia$3text
337 $acomputer$bc$2rdamedia$3CD-ROM
338 $avolume$bnc$2rdacarrier$3text
338 $acomputer disc$bcd$2rdacarrier$3CD-ROM
347 $aimage file$bJPEG$2rda
504 $aIncludes bibliographical references (pages 313-322).
520 $a"1. Mylonites 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?"--Publisher's website.
505 0 $aIntroduction: 1.1. Definition of the term "mylonite" ; 1.2. Classification of mylonites ; 1.3. Determining factors in the formation of mylonites -- Cataclasites -- 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.
650 0 $aMylonite$vAtlases.
700 1 $aPasschier, C. W.$q(Cees W.),$d1954-$eauthor.
700 1 $aWiersma, Dirk J.,$d1939-$eauthor.
856 42 $3Publisher description$uhttp://www.loc.gov/catdir/enhancements/fy1315/2009939942-d.html
856 41 $3Table of contents only$uhttp://www.loc.gov/catdir/enhancements/fy1315/2009939942-t.html