Microstructures in carbonates.

H. R. Wenk; D. J. Barber; R. J. Reeder

Microstructures in carbonates.

H. R. Wenk
, D. J. Barber
, R. J. Reeder

VP for Brookhaven Affairs

Stony Brook University

University of California at Berkeley

Research output: Contribution to journal › Article › peer-review

77 Scopus citations

Abstract

Sedimentary calcites and dolomites are commonly non-stoichiometric and such non-ideality in composition may be accomodated by numerous defects in the structure. The origin of microstructures are discussed and the application of SEM, TEM, scanning TEM and high-resolution EM to the study of carbonates is described in detail. Polymorphic transformations, variations in stacking order, modulated structures parallel to (1014), deformation, dislocations, stacking faults and styolites are all discussed and illustrated. -R.A.H.

Original language	English
Pages (from-to)	301-367
Number of pages	67
Journal	Unknown Journal
Volume	11
State	Published - 1983

Cite this

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title = "Microstructures in carbonates.",

abstract = "Sedimentary calcites and dolomites are commonly non-stoichiometric and such non-ideality in composition may be accomodated by numerous defects in the structure. The origin of microstructures are discussed and the application of SEM, TEM, scanning TEM and high-resolution EM to the study of carbonates is described in detail. Polymorphic transformations, variations in stacking order, modulated structures parallel to (1014), deformation, dislocations, stacking faults and styolites are all discussed and illustrated. -R.A.H.",

author = "Wenk, \{H. R.\} and Barber, \{D. J.\} and Reeder, \{R. J.\}",

year = "1983",

language = "English",

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TY - JOUR

T1 - Microstructures in carbonates.

AU - Wenk, H. R.

AU - Barber, D. J.

AU - Reeder, R. J.

PY - 1983

Y1 - 1983

N2 - Sedimentary calcites and dolomites are commonly non-stoichiometric and such non-ideality in composition may be accomodated by numerous defects in the structure. The origin of microstructures are discussed and the application of SEM, TEM, scanning TEM and high-resolution EM to the study of carbonates is described in detail. Polymorphic transformations, variations in stacking order, modulated structures parallel to (1014), deformation, dislocations, stacking faults and styolites are all discussed and illustrated. -R.A.H.

AB - Sedimentary calcites and dolomites are commonly non-stoichiometric and such non-ideality in composition may be accomodated by numerous defects in the structure. The origin of microstructures are discussed and the application of SEM, TEM, scanning TEM and high-resolution EM to the study of carbonates is described in detail. Polymorphic transformations, variations in stacking order, modulated structures parallel to (1014), deformation, dislocations, stacking faults and styolites are all discussed and illustrated. -R.A.H.

UR - https://www.scopus.com/pages/publications/0021019578

UR - https://www.scopus.com/pages/publications/0020940310

M3 - Article

VL - 11

SP - 301

EP - 367

JO - Unknown Journal

JF - Unknown Journal

ER -

Microstructures in carbonates.

Abstract

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