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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 0 0 _aQE475.M95
_bT76 2010
082 _a552.4
_bTRO-A
100 1 _aTrouw, R. A. J.
_q(Rudolph A. J.),
_d1944-
_eaut
_931911
245 1 0 _aAtlas of mylonites - and related microstructures /
_cRudolph A.J. Trouw, Cees W. Passchier, Dirk J. Wiersma.
300 _a322 pages :
_bcolor illustrations ;
_c29 cm
300 _a1 CD-ROM ;
_c4 3/4 in.
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.
650 0 _aMylonite
_vAtlases.
_931912
700 1 _aPasschier, C. W.
_q(Cees W.),
_d1954-
_eaut
_931913
700 1 _aWiersma, Dirk J.,
_d1939-
_eaut
_931914
264 1 _aHeidelberg ;
_aNew York :
_bSpringer,
_c[2010]
264 4 _c©2010
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).
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.
856 4 2 _3Publisher description
_uhttp://www.loc.gov/catdir/enhancements/fy1315/2009939942-d.html
856 4 1 _3Table of contents only
_uhttp://www.loc.gov/catdir/enhancements/fy1315/2009939942-t.html
906 _a7
_bcbc
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942 _2ddc
_cBK