Geochemical changes accompanying mylonitisation of granite at the base of the Helgeland Nappe Complex, Nord-Trøndelag, central Norway
A progressive conversion of megacrystic granite into mylonites at the base of the Helgeland Nappe Complex in the Caledonides of central Norway is reflected in microstructural, textural and modal changes. These mylonites record a considerable, regional,Scandian thrust deformation followed by a late-S...
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ftnorgesgu:oai:openarchive.ngu.no:11250/2674171 2023-05-15T16:34:07+02:00 Geochemical changes accompanying mylonitisation of granite at the base of the Helgeland Nappe Complex, Nord-Trøndelag, central Norway Roberts, David Nissen, August L. HØYLANDET 18234 Grong 18243 Harran 18244 Kongsmoen GRONG 2006 application/pdf https://hdl.handle.net/11250/2674171 eng eng NGU Bulletin (446) https://hdl.handle.net/11250/2674171 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 35-41 GEOKJEMI MYLONITT GRANITT BERGGRUNNSGEOLOGI Journal article 2006 ftnorgesgu 2022-07-03T15:26:35Z A progressive conversion of megacrystic granite into mylonites at the base of the Helgeland Nappe Complex in the Caledonides of central Norway is reflected in microstructural, textural and modal changes. These mylonites record a considerable, regional,Scandian thrust deformation followed by a late-Scandian phase of major extension. The chemical changes that accompanied the structural and mineralogical conversion are also quite significant. Major oxides generally show wt.% losses (e.g.,Al2O3down >12% and CaO 50%) except for SiO2 which gains 10%,partly reflecting a twofold increase in modal quartz. Of the trace elements, Sr and Ba fall markedly, up to 60%, a feature that reflects their affinity for the modally diminishing feldspars (65 vol.% in granite to <20 vol.% in mylonites). An application of normalised mylonite\/protolith ratio plots for selected oxides indicates that this regionally important mylonitic shear zone is of the volume-gain\/isovolume variety. Such volume-gain systems, commonly involving fluid-enhanced silicification, are more typical of extensional shear situations. These results conform well with the regional structural picture wherein the major, extensional, late-Scandian, Kollstraumen detachment zone occurs in the footwall to the mylonitic base of the Helgeland Nappe Complex; and extensional structures overprint the thrust fabric in the mylonitised granite. 56205 Article in Journal/Newspaper Helgeland NGU Open Archive (Geological Survey of Norway) Harran ENVELOPE(12.486,12.486,64.559,64.559) Helgeland Høylandet ENVELOPE(12.300,12.300,64.628,64.628) Kollstraumen ENVELOPE(12.177,12.177,65.041,65.041) Kongsmoen ENVELOPE(12.435,12.435,64.882,64.882) Norway |
institution |
Open Polar |
collection |
NGU Open Archive (Geological Survey of Norway) |
op_collection_id |
ftnorgesgu |
language |
English |
topic |
GEOKJEMI MYLONITT GRANITT BERGGRUNNSGEOLOGI |
spellingShingle |
GEOKJEMI MYLONITT GRANITT BERGGRUNNSGEOLOGI Roberts, David Nissen, August L. Geochemical changes accompanying mylonitisation of granite at the base of the Helgeland Nappe Complex, Nord-Trøndelag, central Norway |
topic_facet |
GEOKJEMI MYLONITT GRANITT BERGGRUNNSGEOLOGI |
description |
A progressive conversion of megacrystic granite into mylonites at the base of the Helgeland Nappe Complex in the Caledonides of central Norway is reflected in microstructural, textural and modal changes. These mylonites record a considerable, regional,Scandian thrust deformation followed by a late-Scandian phase of major extension. The chemical changes that accompanied the structural and mineralogical conversion are also quite significant. Major oxides generally show wt.% losses (e.g.,Al2O3down >12% and CaO 50%) except for SiO2 which gains 10%,partly reflecting a twofold increase in modal quartz. Of the trace elements, Sr and Ba fall markedly, up to 60%, a feature that reflects their affinity for the modally diminishing feldspars (65 vol.% in granite to <20 vol.% in mylonites). An application of normalised mylonite\/protolith ratio plots for selected oxides indicates that this regionally important mylonitic shear zone is of the volume-gain\/isovolume variety. Such volume-gain systems, commonly involving fluid-enhanced silicification, are more typical of extensional shear situations. These results conform well with the regional structural picture wherein the major, extensional, late-Scandian, Kollstraumen detachment zone occurs in the footwall to the mylonitic base of the Helgeland Nappe Complex; and extensional structures overprint the thrust fabric in the mylonitised granite. 56205 |
format |
Article in Journal/Newspaper |
author |
Roberts, David Nissen, August L. |
author_facet |
Roberts, David Nissen, August L. |
author_sort |
Roberts, David |
title |
Geochemical changes accompanying mylonitisation of granite at the base of the Helgeland Nappe Complex, Nord-Trøndelag, central Norway |
title_short |
Geochemical changes accompanying mylonitisation of granite at the base of the Helgeland Nappe Complex, Nord-Trøndelag, central Norway |
title_full |
Geochemical changes accompanying mylonitisation of granite at the base of the Helgeland Nappe Complex, Nord-Trøndelag, central Norway |
title_fullStr |
Geochemical changes accompanying mylonitisation of granite at the base of the Helgeland Nappe Complex, Nord-Trøndelag, central Norway |
title_full_unstemmed |
Geochemical changes accompanying mylonitisation of granite at the base of the Helgeland Nappe Complex, Nord-Trøndelag, central Norway |
title_sort |
geochemical changes accompanying mylonitisation of granite at the base of the helgeland nappe complex, nord-trøndelag, central norway |
publishDate |
2006 |
url |
https://hdl.handle.net/11250/2674171 |
op_coverage |
HØYLANDET 18234 Grong 18243 Harran 18244 Kongsmoen GRONG |
long_lat |
ENVELOPE(12.486,12.486,64.559,64.559) ENVELOPE(12.300,12.300,64.628,64.628) ENVELOPE(12.177,12.177,65.041,65.041) ENVELOPE(12.435,12.435,64.882,64.882) |
geographic |
Harran Helgeland Høylandet Kollstraumen Kongsmoen Norway |
geographic_facet |
Harran Helgeland Høylandet Kollstraumen Kongsmoen Norway |
genre |
Helgeland |
genre_facet |
Helgeland |
op_source |
35-41 |
op_relation |
NGU Bulletin (446) https://hdl.handle.net/11250/2674171 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
_version_ |
1766023865550503936 |