Distinguishing syn-cleavage folds from pre-cleavage folds to which cleavage is virtually axial planar: examples from the Cambrian core of the Lower Palaeozoic Anglo-Brabant Deformation Belt (Belgium)

Within the Cambrian Jodoigne Formation in the easternmost part of the Anglo-Brabant Deformation Belt, sub-horizontal to gently plunging folds occur within the limbs of steeply plunging folds. The latter folds are cogenetic with cleavage and are attributed to the Brabantian deformation event. In cont...

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Published in:Journal of Structural Geology
Main Authors: Debacker, T, Van Noorden, Michiel, Sintubin, Manuel
Format: Article in Journal/Newspaper
Language:English
Published: Pergamon-elsevier science ltd 2006
Subjects:
Online Access:https://lirias.kuleuven.be/handle/123456789/76521
http://gateway.newisiknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=CCC&SrcApp=PRODUCT_NAME&SrcURL=WOS_RETURN_URL&CKEY=DEBA1123060028JT&DestLinkType=FullRecord&DestApp=CCC&SrcDesc=RETURN_ALT_TEXT&SrcAppSID=APP_SID
https://doi.org/10.1016/j.jsg.2006.03.027
https://lirias.kuleuven.be/bitstream/123456789/76521/1//JSG-Debackeretal2006.pdf
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spelling ftunivleuven:oai:lirias.kuleuven.be:123456789/76521 2023-05-15T17:22:22+02:00 Distinguishing syn-cleavage folds from pre-cleavage folds to which cleavage is virtually axial planar: examples from the Cambrian core of the Lower Palaeozoic Anglo-Brabant Deformation Belt (Belgium) Debacker, T Van Noorden, Michiel Sintubin, Manuel 2006 https://lirias.kuleuven.be/handle/123456789/76521 http://gateway.newisiknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=CCC&SrcApp=PRODUCT_NAME&SrcURL=WOS_RETURN_URL&CKEY=DEBA1123060028JT&DestLinkType=FullRecord&DestApp=CCC&SrcDesc=RETURN_ALT_TEXT&SrcAppSID=APP_SID https://doi.org/10.1016/j.jsg.2006.03.027 https://lirias.kuleuven.be/bitstream/123456789/76521/1//JSG-Debackeretal2006.pdf en eng Pergamon-elsevier science ltd Journal of structural geology vol:28 issue:7 pages:1123-1138 https://lirias.kuleuven.be/handle/123456789/76521 0191-8141 http://gateway.newisiknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=CCC&SrcApp=PRODUCT_NAME&SrcURL=WOS_RETURN_URL&CKEY=DEBA1123060028JT&DestLinkType=FullRecord&DestApp=CCC&SrcDesc=RETURN_ALT_TEXT&SrcAppSID=APP_SID http://dx.doi.org/10.1016/j.jsg.2006.03.027 https://lirias.kuleuven.be/bitstream/123456789/76521/1//JSG-Debackeretal2006.pdf 28763;intranet avalonia cleavage fanning cleavage refraction lower palaeozoic slate belt slump fold northeastern-newfoundland-appalachians slump folds transected folds patterns massif flysch beds Article IT 28763;Article 2006 ftunivleuven https://doi.org/10.1016/j.jsg.2006.03.027 2017-06-02T19:11:15Z Within the Cambrian Jodoigne Formation in the easternmost part of the Anglo-Brabant Deformation Belt, sub-horizontal to gently plunging folds occur within the limbs of steeply plunging folds. The latter folds are cogenetic with cleavage and are attributed to the Brabantian deformation event. In contrast, although cleavage is also (1) virtually axial planar to the sub-horizontal to gently plunging higher-order folds, shows (2) a well-developed divergent fanning across these folds, (3) an opposing sense of cleavage refraction on opposite fold limbs, and (4) only very small cleavage transection angles, an analysis of the cleavage/bedding intersection lineation suggests that these higher-order folds have a pre-cleavage origin. On the basis of a comparison of structural and sedimentological features these higher-order folds are interpreted as slump folds. The seemingly 'normal' cleavage/fold relationship across the slump folds within the limbs of the large steeply plunging folds is due to the very small angle between cleavage and bedding. status: published Article in Journal/Newspaper Newfoundland KU Leuven: Lirias Fanning ENVELOPE(-60.632,-60.632,-72.404,-72.404) Journal of Structural Geology 28 7 1123 1138
institution Open Polar
collection KU Leuven: Lirias
op_collection_id ftunivleuven
language English
topic avalonia
cleavage fanning
cleavage refraction
lower palaeozoic
slate belt
slump fold
northeastern-newfoundland-appalachians
slump folds
transected folds
patterns
massif
flysch
beds
spellingShingle avalonia
cleavage fanning
cleavage refraction
lower palaeozoic
slate belt
slump fold
northeastern-newfoundland-appalachians
slump folds
transected folds
patterns
massif
flysch
beds
Debacker, T
Van Noorden, Michiel
Sintubin, Manuel
Distinguishing syn-cleavage folds from pre-cleavage folds to which cleavage is virtually axial planar: examples from the Cambrian core of the Lower Palaeozoic Anglo-Brabant Deformation Belt (Belgium)
topic_facet avalonia
cleavage fanning
cleavage refraction
lower palaeozoic
slate belt
slump fold
northeastern-newfoundland-appalachians
slump folds
transected folds
patterns
massif
flysch
beds
description Within the Cambrian Jodoigne Formation in the easternmost part of the Anglo-Brabant Deformation Belt, sub-horizontal to gently plunging folds occur within the limbs of steeply plunging folds. The latter folds are cogenetic with cleavage and are attributed to the Brabantian deformation event. In contrast, although cleavage is also (1) virtually axial planar to the sub-horizontal to gently plunging higher-order folds, shows (2) a well-developed divergent fanning across these folds, (3) an opposing sense of cleavage refraction on opposite fold limbs, and (4) only very small cleavage transection angles, an analysis of the cleavage/bedding intersection lineation suggests that these higher-order folds have a pre-cleavage origin. On the basis of a comparison of structural and sedimentological features these higher-order folds are interpreted as slump folds. The seemingly 'normal' cleavage/fold relationship across the slump folds within the limbs of the large steeply plunging folds is due to the very small angle between cleavage and bedding. status: published
format Article in Journal/Newspaper
author Debacker, T
Van Noorden, Michiel
Sintubin, Manuel
author_facet Debacker, T
Van Noorden, Michiel
Sintubin, Manuel
author_sort Debacker, T
title Distinguishing syn-cleavage folds from pre-cleavage folds to which cleavage is virtually axial planar: examples from the Cambrian core of the Lower Palaeozoic Anglo-Brabant Deformation Belt (Belgium)
title_short Distinguishing syn-cleavage folds from pre-cleavage folds to which cleavage is virtually axial planar: examples from the Cambrian core of the Lower Palaeozoic Anglo-Brabant Deformation Belt (Belgium)
title_full Distinguishing syn-cleavage folds from pre-cleavage folds to which cleavage is virtually axial planar: examples from the Cambrian core of the Lower Palaeozoic Anglo-Brabant Deformation Belt (Belgium)
title_fullStr Distinguishing syn-cleavage folds from pre-cleavage folds to which cleavage is virtually axial planar: examples from the Cambrian core of the Lower Palaeozoic Anglo-Brabant Deformation Belt (Belgium)
title_full_unstemmed Distinguishing syn-cleavage folds from pre-cleavage folds to which cleavage is virtually axial planar: examples from the Cambrian core of the Lower Palaeozoic Anglo-Brabant Deformation Belt (Belgium)
title_sort distinguishing syn-cleavage folds from pre-cleavage folds to which cleavage is virtually axial planar: examples from the cambrian core of the lower palaeozoic anglo-brabant deformation belt (belgium)
publisher Pergamon-elsevier science ltd
publishDate 2006
url https://lirias.kuleuven.be/handle/123456789/76521
http://gateway.newisiknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=CCC&SrcApp=PRODUCT_NAME&SrcURL=WOS_RETURN_URL&CKEY=DEBA1123060028JT&DestLinkType=FullRecord&DestApp=CCC&SrcDesc=RETURN_ALT_TEXT&SrcAppSID=APP_SID
https://doi.org/10.1016/j.jsg.2006.03.027
https://lirias.kuleuven.be/bitstream/123456789/76521/1//JSG-Debackeretal2006.pdf
long_lat ENVELOPE(-60.632,-60.632,-72.404,-72.404)
geographic Fanning
geographic_facet Fanning
genre Newfoundland
genre_facet Newfoundland
op_relation Journal of structural geology vol:28 issue:7 pages:1123-1138
https://lirias.kuleuven.be/handle/123456789/76521
0191-8141
http://gateway.newisiknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=CCC&SrcApp=PRODUCT_NAME&SrcURL=WOS_RETURN_URL&CKEY=DEBA1123060028JT&DestLinkType=FullRecord&DestApp=CCC&SrcDesc=RETURN_ALT_TEXT&SrcAppSID=APP_SID
http://dx.doi.org/10.1016/j.jsg.2006.03.027
https://lirias.kuleuven.be/bitstream/123456789/76521/1//JSG-Debackeretal2006.pdf
op_rights 28763;intranet
op_doi https://doi.org/10.1016/j.jsg.2006.03.027
container_title Journal of Structural Geology
container_volume 28
container_issue 7
container_start_page 1123
op_container_end_page 1138
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