MOTS EN ANGLAIS EN RAPPORT AVEC «STYLOLITIC»
stylolitic
stylolitic
define
irregular
columnar
structure
certain
limestones
columns
being
approximately
right
angles
bedding
planes
reverso
meaning
also
stylitic
stylistic
stylolite
stylistics
vocabulary
nature
origin
jstor
tennessee
marble
limestone
york
bedford
indiana
character
urban
stylites
styll
styllin
styllz
stylmish
stylo
stylobate
stylol
stylophage
stylus
nail
stymie
stymied
stymiee
defined
cleavage
refraction
lower
paleozoic
closely
spaced
developed
closures
folds
carbonate
rocks
great
valley
west
10 LIVRES EN ANGLAIS EN RAPPORT AVEC «STYLOLITIC»
Découvrez l'usage de
stylolitic dans la sélection bibliographique suivante. Des livres en rapport avec
stylolitic et de courts extraits de ceux-ci pour replacer dans son contexte son utilisation littéraire.
1
Principles of Rock Deformation
STYLOLITIC JOINTS Stylolitic joints are rough surfaces finely covered with little
peaks, the stylolites which are outlined by a concentration of phyllitic and opaque
minerals (fig. 5. 9). These Joints are particularly common in limestones where ...
Adolphe Nicolas, D. H. Mainprice, 1987
2
Analysis of Geological Structures
These cleavages, which are respectively termed stylolitic, anastomosing, rough
and smooth, are shown in Fig. 17.3. Microlithon fabric Another subdivision of
spaced cleavage can be made on the basis of whether or not there is a preferred
...
Neville J. Price, John W. Cosgrove, 1990
3
Quartz Cementation in Sandstones: Special Publication 29 of ...
seconds using the cold-cathode luminoscope, but shows similar slow decay in
the hot-cathode device as quartz cement outside stylolites. Stylolitic quartz
crystals commonly show inclusion-rich inner areas in normal transmitted light, but
with ...
R. Worden, Sadoon Morad, 2009
4
Carbonate Reservoir Characterization: An Integrated Approach
Rock-fabric types A, B, and C, and thin stylolitic beds are distributed within the 10
high-frequency cycles. Low porosity layers (dense layers) within rock-fabric type
C are located at the base of cycles A6, B1, and B3. The second step in this ...
5
Whence the Mountains?: Inquiries Into the Evolution of ...
Stylolitic fractures are significantly more common than grikes in the area, but
because the grikes pass laterally and vertically into stylolitic fractures, they
comprise a single genetic set of fractures, only some of which were karst-
widened before ...
James W. Sears, Tekla A. Harms, C. A. Evenchick, 2007
6
From Precambrian Rift Volcanoes to the Mississippian Shelf ...
and both may or may not be stylolitic. When Carthage and Phenix stone was
originally cut into slabs by means of gang saws in the early 1900s, the cuts were
made parallel to bedding. Later, both stones were also cut perpendicular to
bedding.
Kevin R. Evans, James S. Aber, 2010
7
The Circum-Gulf of Mexico and the Caribbean: Hydrocarbon ...
(F) Outcrop view of massive limestone with black chert nodules and bed-parallel
stylolites (Atoyac anticline). sequences devoid of any major shaly interbeds (
Plate IIIF), and stylolitic planes perpendicular to the bedding and coeval with ...
Claudio Bartolini, Richard T. Buffler, Jon Frederic Blickwede, 2003
8
Geometries and mechanisms of thrusting, with special ...
Figure 8. Microscopic F2 cut by axial-planar 82, which has the same sense of
offset on both fold limbs. antiform but in the core of the fold, within a few meters of
the axial surface, they are locally remarkably stylolitic (Fig. 7b). These folia are ...
9
Geological Survey Bulletin
Bituminous, stylolitic, and fossiliferous. Algal material with silicious coating;
stylolites. Sphalerite has replaced dolomite at 11.8 and 12.0 ft, in algae at 13.0 ft.
Strong bituminous odor. Oak Orchard member of Howell and Sanford: 0.0- 9.0
9.0- ...
10
Building Stone Decay: From Diagnosis to Conservation
This can be explained by its extremely dense micritic structure (Fig. 2).
Nevertheless. Kirmenjak is visually and petrographically characterized by
horizontal stylolitic discontinuities (Fig. 2). Stylolites represent an anisotropic
feature of the stone, ...
European Geosciences Union. General Assembly, Richard Přikryl, Bernard J. Smith, 2007
