PALABRAS DEL INGLÉS RELACIONADAS CON «CENTROCLINAL»
centroclinal
centroclinal
meaning
pronunciation
translations
merriam
webster
dipping
toward
common
point
center
opposed
quaquaversal
origin
centr
clinal
this
word
doesn
usually
appear
collins
always
adjective
geology
relating
designating
rock
formation
which
strata
slope
down
towards
central
area
define
reverso
also
centrolecithal
locking
centrically
centrical
definitions
onelook
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found
dictionaries
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that
include
click
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directly
page
where
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finder
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ending
letter
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anagrams
starting
centroclinalの意味
英和辞典
weblio辞書
centroclinalの意味や和訳。
ドーム状の
万語ある英和辞典・和英辞典。発音・
イディオムも分かる英語辞書。centroclinal
fold
results
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TENDENCIAS DE USO ACTUALES DEL TÉRMINO «CENTROCLINAL»
El término «centroclinal» apenas se utiliza habitualmente y ocupa la posición
202.764 de nuestra lista de términos más usados del
diccionario de inglés.
En el mapa anterior se refleja la frecuencia de uso del término «centroclinal» en los diferentes paises.
Principales tendencias de búsqueda y usos comunes de
centroclinal
Listado de las príncipales búsquedas realizadas por los usuarios para acceder a nuestro
diccionario de inglés en línea y expresiones más usadas con la palabra «centroclinal».
10 LIBROS DEL INGLÉS RELACIONADOS CON «CENTROCLINAL»
Descubre el uso de
centroclinal en la siguiente selección bibliográfica. Libros relacionados con
centroclinal y pequeños extractos de los mismos para contextualizar su uso en la literatura.
The centroclinal fold or structural basin is a special case of a syncline, in which
the beds dip inward from all sides towards a central point (Fig. 75). Both domes (
quaquaversal folds) and basins (centroclinal folds) are regarded as modifications
...
Heinrich Ries, Thomas L. Watson
Cf: periclinal Igeol]. centroclinal fold centrocline. centrocline (cen'-tro-cline) An
equidimensional basin characteristic of cratonic areas, in which the strata dip
towards a central low point. The term is little used in the U.S. Cf: pericline Istruc
geol].
Julia A. Jackson, James P. Mehl, Klaus K. E. Neuendorf, 2005
M.R. LEEDER, M. NAMI , A.C. SCOTT and A. GARDINER SUMMARY
Centroclinal cross strata have been examined around an in situ tree trunk in
Westphalian B rocks of West Yorkshire. The structures were probably initiated by
scour during ...
And there is another word, 'centroclinal', which has the definition of being 'the
opposite of quaquaversal'. " Genesis smiles and looks rather pleased with
himself. The language creaks and finds it hard to cope. Trans Media loved
playing with ...
Attention is drawn to evidence of considerable movements resulting in almost
symmetrical oval basins or centroclinal folds. The F undamental Strata which are
at or very near the surface “have very definite relationships, both to the
centroclinal ...
6
Crustal Structures and Mineral Deposits: E.S.T. O'Driscoll's ...
... contemporaneous centroclinal deformation. A full treatment of cross folding
concepts is beyond the scope of this paper. The reader should refer to the very
informative paper by Whitten (25) for extensive references to cross folding dating
as ...
Jennifer Anne Bourne, 2007
7
Rebels and Devils: The Psychology of Liberation
Quaquaversal—Pointing in every direction similtaneously. In the dictionary
centroclinal is defined as the opposite of quaquaversal. Sigil—For the purposes
of this essay, defined as a 2–3 dimensional product or ideagram; consciously
invoking ...
Christopher S. Hyatt, 2008
8
The Geological Record of Neoproterozoic Glaciations
... Nichatka Formation are located in the southem centroclinal part of the marginal
Berezovskaya basin of the Siberian craton. Deposits of the gently sloping
southeastem limb of the asymmetrical basin are unaltered. whereas those of the
steep.
Emmanuelle Arnaud, Galen P. Halverson, Graham Shields-Zhou, 2011
... by the squeezing out of plastic core material, sometimes piercing through the
surface. The opposite of dome is a structural basin that is a synclinal structure in
which the beds are centroclinal, that is, they dip inwards towards the centre ...
10
Geological Survey Bulletin
... a second, intersecting, less extensive system trends mostly N. 50°-80° E. and
dips nearly vertically; and third, a locally mineralized, low-dipping (mostly less
than 30°) centroclinal system of partly sheared joints is west of Little Myrtle Lake (
fig.
