Palaeozoic flysch series in the Coastal Cordillera of Northern Chile

Abstract A discontinuous outcrop of Palaeozoic rhythmic clastites appears in the North Chilean Coastal Cordillera. The Formación El Toco (21°15′–22°15′S) whose scarce flora points to a presumably Upper Devonian age forms the northernmost part of the outcrop. It is discordantly overlain by Lower Jura...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Breitkreuz, Christoph [verfasserIn] Bahlburg, Heinrich

Format:	Artikel
Sprache:	Englisch

Erschienen:	1985

Schlagwörter:	Jurassic Devonian Detritus Turbidite Lower Jurassic

Anmerkung:	© Ferdinand Enke Verlag Stuttgart 1985

Übergeordnetes Werk:	Enthalten in: Geologische Rundschau - Springer-Verlag, 1910, 74(1985), 3 vom: Okt., Seite 565-572
Übergeordnetes Werk:	volume:74 ; year:1985 ; number:3 ; month:10 ; pages:565-572

Links:	Volltext

DOI / URN:	10.1007/BF01821212

Katalog-ID:	OLC2070404218

Internformat


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520			\|a Abstract A discontinuous outcrop of Palaeozoic rhythmic clastites appears in the North Chilean Coastal Cordillera. The Formación El Toco (21°15′–22°15′S) whose scarce flora points to a presumably Upper Devonian age forms the northernmost part of the outcrop. It is discordantly overlain by Lower Jurassic volcanics (Fm. La Negra), its base, however, is not exposed. Hercynian heteromorphous deformation led to predominantly NW trending folds strongly inclined mostly to the SW. Chevron-like folds of 0.1 to 30 m occur locally and seem to display properties transitional between synsedimentary-gravitational and early tectonic deformation. The series which is at least 2300 m thick consists of proximal, in parts pebbly turbidites with non-turbiditic finegrained intercalations. Incomplete BOUMA-sequences frequently begin with A-beds of grey to green immature, badly sorted coarse sandstones of up to 6 m thickness containing isolated quartz- and pelite-clasts. Measurements of flute casts and f oresets show palaeocurrents which came from NW and NNE. Along with petrographic observations they indicate southward directed transport of detritus from low metamorphic sedimentary and magmatic source areas into an Upper Devonian nonvolcanic basin.
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Indexfelder

author_variant	c b cb h b hb
matchkey_str	article:00167835:1985----::aaooclsheisnhcatlodle
hierarchy_sort_str	1985
publishDate	1985
allfields	10.1007/BF01821212 doi (DE-627)OLC2070404218 (DE-He213)BF01821212-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Breitkreuz, Christoph verfasserin aut Palaeozoic flysch series in the Coastal Cordillera of Northern Chile 1985 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1985 Abstract A discontinuous outcrop of Palaeozoic rhythmic clastites appears in the North Chilean Coastal Cordillera. The Formación El Toco (21°15′–22°15′S) whose scarce flora points to a presumably Upper Devonian age forms the northernmost part of the outcrop. It is discordantly overlain by Lower Jurassic volcanics (Fm. La Negra), its base, however, is not exposed. Hercynian heteromorphous deformation led to predominantly NW trending folds strongly inclined mostly to the SW. Chevron-like folds of 0.1 to 30 m occur locally and seem to display properties transitional between synsedimentary-gravitational and early tectonic deformation. The series which is at least 2300 m thick consists of proximal, in parts pebbly turbidites with non-turbiditic finegrained intercalations. Incomplete BOUMA-sequences frequently begin with A-beds of grey to green immature, badly sorted coarse sandstones of up to 6 m thickness containing isolated quartz- and pelite-clasts. Measurements of flute casts and f oresets show palaeocurrents which came from NW and NNE. Along with petrographic observations they indicate southward directed transport of detritus from low metamorphic sedimentary and magmatic source areas into an Upper Devonian nonvolcanic basin. Jurassic Devonian Detritus Turbidite Lower Jurassic Bahlburg, Heinrich aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 74(1985), 3 vom: Okt., Seite 565-572 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:74 year:1985 number:3 month:10 pages:565-572 https://doi.org/10.1007/BF01821212 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 74 1985 3 10 565-572
spelling	10.1007/BF01821212 doi (DE-627)OLC2070404218 (DE-He213)BF01821212-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Breitkreuz, Christoph verfasserin aut Palaeozoic flysch series in the Coastal Cordillera of Northern Chile 1985 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1985 Abstract A discontinuous outcrop of Palaeozoic rhythmic clastites appears in the North Chilean Coastal Cordillera. The Formación El Toco (21°15′–22°15′S) whose scarce flora points to a presumably Upper Devonian age forms the northernmost part of the outcrop. It is discordantly overlain by Lower Jurassic volcanics (Fm. La Negra), its base, however, is not exposed. Hercynian heteromorphous deformation led to predominantly NW trending folds strongly inclined mostly to the SW. Chevron-like folds of 0.1 to 30 m occur locally and seem to display properties transitional between synsedimentary-gravitational and early tectonic deformation. The series which is at least 2300 m thick consists of proximal, in parts pebbly turbidites with non-turbiditic finegrained intercalations. Incomplete BOUMA-sequences frequently begin with A-beds of grey to green immature, badly sorted coarse sandstones of up to 6 m thickness containing isolated quartz- and pelite-clasts. Measurements of flute casts and f oresets show palaeocurrents which came from NW and NNE. Along with petrographic observations they indicate southward directed transport of detritus from low metamorphic sedimentary and magmatic source areas into an Upper Devonian nonvolcanic basin. Jurassic Devonian Detritus Turbidite Lower Jurassic Bahlburg, Heinrich aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 74(1985), 3 vom: Okt., Seite 565-572 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:74 year:1985 number:3 month:10 pages:565-572 https://doi.org/10.1007/BF01821212 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 74 1985 3 10 565-572
allfields_unstemmed	10.1007/BF01821212 doi (DE-627)OLC2070404218 (DE-He213)BF01821212-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Breitkreuz, Christoph verfasserin aut Palaeozoic flysch series in the Coastal Cordillera of Northern Chile 1985 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1985 Abstract A discontinuous outcrop of Palaeozoic rhythmic clastites appears in the North Chilean Coastal Cordillera. The Formación El Toco (21°15′–22°15′S) whose scarce flora points to a presumably Upper Devonian age forms the northernmost part of the outcrop. It is discordantly overlain by Lower Jurassic volcanics (Fm. La Negra), its base, however, is not exposed. Hercynian heteromorphous deformation led to predominantly NW trending folds strongly inclined mostly to the SW. Chevron-like folds of 0.1 to 30 m occur locally and seem to display properties transitional between synsedimentary-gravitational and early tectonic deformation. The series which is at least 2300 m thick consists of proximal, in parts pebbly turbidites with non-turbiditic finegrained intercalations. Incomplete BOUMA-sequences frequently begin with A-beds of grey to green immature, badly sorted coarse sandstones of up to 6 m thickness containing isolated quartz- and pelite-clasts. Measurements of flute casts and f oresets show palaeocurrents which came from NW and NNE. Along with petrographic observations they indicate southward directed transport of detritus from low metamorphic sedimentary and magmatic source areas into an Upper Devonian nonvolcanic basin. Jurassic Devonian Detritus Turbidite Lower Jurassic Bahlburg, Heinrich aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 74(1985), 3 vom: Okt., Seite 565-572 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:74 year:1985 number:3 month:10 pages:565-572 https://doi.org/10.1007/BF01821212 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 74 1985 3 10 565-572
allfieldsGer	10.1007/BF01821212 doi (DE-627)OLC2070404218 (DE-He213)BF01821212-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Breitkreuz, Christoph verfasserin aut Palaeozoic flysch series in the Coastal Cordillera of Northern Chile 1985 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1985 Abstract A discontinuous outcrop of Palaeozoic rhythmic clastites appears in the North Chilean Coastal Cordillera. The Formación El Toco (21°15′–22°15′S) whose scarce flora points to a presumably Upper Devonian age forms the northernmost part of the outcrop. It is discordantly overlain by Lower Jurassic volcanics (Fm. La Negra), its base, however, is not exposed. Hercynian heteromorphous deformation led to predominantly NW trending folds strongly inclined mostly to the SW. Chevron-like folds of 0.1 to 30 m occur locally and seem to display properties transitional between synsedimentary-gravitational and early tectonic deformation. The series which is at least 2300 m thick consists of proximal, in parts pebbly turbidites with non-turbiditic finegrained intercalations. Incomplete BOUMA-sequences frequently begin with A-beds of grey to green immature, badly sorted coarse sandstones of up to 6 m thickness containing isolated quartz- and pelite-clasts. Measurements of flute casts and f oresets show palaeocurrents which came from NW and NNE. Along with petrographic observations they indicate southward directed transport of detritus from low metamorphic sedimentary and magmatic source areas into an Upper Devonian nonvolcanic basin. Jurassic Devonian Detritus Turbidite Lower Jurassic Bahlburg, Heinrich aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 74(1985), 3 vom: Okt., Seite 565-572 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:74 year:1985 number:3 month:10 pages:565-572 https://doi.org/10.1007/BF01821212 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 74 1985 3 10 565-572
allfieldsSound	10.1007/BF01821212 doi (DE-627)OLC2070404218 (DE-He213)BF01821212-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Breitkreuz, Christoph verfasserin aut Palaeozoic flysch series in the Coastal Cordillera of Northern Chile 1985 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1985 Abstract A discontinuous outcrop of Palaeozoic rhythmic clastites appears in the North Chilean Coastal Cordillera. The Formación El Toco (21°15′–22°15′S) whose scarce flora points to a presumably Upper Devonian age forms the northernmost part of the outcrop. It is discordantly overlain by Lower Jurassic volcanics (Fm. La Negra), its base, however, is not exposed. Hercynian heteromorphous deformation led to predominantly NW trending folds strongly inclined mostly to the SW. Chevron-like folds of 0.1 to 30 m occur locally and seem to display properties transitional between synsedimentary-gravitational and early tectonic deformation. The series which is at least 2300 m thick consists of proximal, in parts pebbly turbidites with non-turbiditic finegrained intercalations. Incomplete BOUMA-sequences frequently begin with A-beds of grey to green immature, badly sorted coarse sandstones of up to 6 m thickness containing isolated quartz- and pelite-clasts. Measurements of flute casts and f oresets show palaeocurrents which came from NW and NNE. Along with petrographic observations they indicate southward directed transport of detritus from low metamorphic sedimentary and magmatic source areas into an Upper Devonian nonvolcanic basin. Jurassic Devonian Detritus Turbidite Lower Jurassic Bahlburg, Heinrich aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 74(1985), 3 vom: Okt., Seite 565-572 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:74 year:1985 number:3 month:10 pages:565-572 https://doi.org/10.1007/BF01821212 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 74 1985 3 10 565-572
language	English
source	Enthalten in Geologische Rundschau 74(1985), 3 vom: Okt., Seite 565-572 volume:74 year:1985 number:3 month:10 pages:565-572
sourceStr	Enthalten in Geologische Rundschau 74(1985), 3 vom: Okt., Seite 565-572 volume:74 year:1985 number:3 month:10 pages:565-572
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Jurassic Devonian Detritus Turbidite Lower Jurassic
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container_title	Geologische Rundschau
authorswithroles_txt_mv	Breitkreuz, Christoph @@aut@@ Bahlburg, Heinrich @@aut@@
publishDateDaySort_date	1985-10-01T00:00:00Z
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author	Breitkreuz, Christoph
spellingShingle	Breitkreuz, Christoph ddc 550 ssgn 13 misc Jurassic misc Devonian misc Detritus misc Turbidite misc Lower Jurassic Palaeozoic flysch series in the Coastal Cordillera of Northern Chile
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topic_title	550 VZ 13 ssgn Palaeozoic flysch series in the Coastal Cordillera of Northern Chile Jurassic Devonian Detritus Turbidite Lower Jurassic
topic	ddc 550 ssgn 13 misc Jurassic misc Devonian misc Detritus misc Turbidite misc Lower Jurassic
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title	Palaeozoic flysch series in the Coastal Cordillera of Northern Chile
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title_full	Palaeozoic flysch series in the Coastal Cordillera of Northern Chile
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title_sort	palaeozoic flysch series in the coastal cordillera of northern chile
title_auth	Palaeozoic flysch series in the Coastal Cordillera of Northern Chile
abstract	Abstract A discontinuous outcrop of Palaeozoic rhythmic clastites appears in the North Chilean Coastal Cordillera. The Formación El Toco (21°15′–22°15′S) whose scarce flora points to a presumably Upper Devonian age forms the northernmost part of the outcrop. It is discordantly overlain by Lower Jurassic volcanics (Fm. La Negra), its base, however, is not exposed. Hercynian heteromorphous deformation led to predominantly NW trending folds strongly inclined mostly to the SW. Chevron-like folds of 0.1 to 30 m occur locally and seem to display properties transitional between synsedimentary-gravitational and early tectonic deformation. The series which is at least 2300 m thick consists of proximal, in parts pebbly turbidites with non-turbiditic finegrained intercalations. Incomplete BOUMA-sequences frequently begin with A-beds of grey to green immature, badly sorted coarse sandstones of up to 6 m thickness containing isolated quartz- and pelite-clasts. Measurements of flute casts and f oresets show palaeocurrents which came from NW and NNE. Along with petrographic observations they indicate southward directed transport of detritus from low metamorphic sedimentary and magmatic source areas into an Upper Devonian nonvolcanic basin. © Ferdinand Enke Verlag Stuttgart 1985
abstractGer	Abstract A discontinuous outcrop of Palaeozoic rhythmic clastites appears in the North Chilean Coastal Cordillera. The Formación El Toco (21°15′–22°15′S) whose scarce flora points to a presumably Upper Devonian age forms the northernmost part of the outcrop. It is discordantly overlain by Lower Jurassic volcanics (Fm. La Negra), its base, however, is not exposed. Hercynian heteromorphous deformation led to predominantly NW trending folds strongly inclined mostly to the SW. Chevron-like folds of 0.1 to 30 m occur locally and seem to display properties transitional between synsedimentary-gravitational and early tectonic deformation. The series which is at least 2300 m thick consists of proximal, in parts pebbly turbidites with non-turbiditic finegrained intercalations. Incomplete BOUMA-sequences frequently begin with A-beds of grey to green immature, badly sorted coarse sandstones of up to 6 m thickness containing isolated quartz- and pelite-clasts. Measurements of flute casts and f oresets show palaeocurrents which came from NW and NNE. Along with petrographic observations they indicate southward directed transport of detritus from low metamorphic sedimentary and magmatic source areas into an Upper Devonian nonvolcanic basin. © Ferdinand Enke Verlag Stuttgart 1985
abstract_unstemmed	Abstract A discontinuous outcrop of Palaeozoic rhythmic clastites appears in the North Chilean Coastal Cordillera. The Formación El Toco (21°15′–22°15′S) whose scarce flora points to a presumably Upper Devonian age forms the northernmost part of the outcrop. It is discordantly overlain by Lower Jurassic volcanics (Fm. La Negra), its base, however, is not exposed. Hercynian heteromorphous deformation led to predominantly NW trending folds strongly inclined mostly to the SW. Chevron-like folds of 0.1 to 30 m occur locally and seem to display properties transitional between synsedimentary-gravitational and early tectonic deformation. The series which is at least 2300 m thick consists of proximal, in parts pebbly turbidites with non-turbiditic finegrained intercalations. Incomplete BOUMA-sequences frequently begin with A-beds of grey to green immature, badly sorted coarse sandstones of up to 6 m thickness containing isolated quartz- and pelite-clasts. Measurements of flute casts and f oresets show palaeocurrents which came from NW and NNE. Along with petrographic observations they indicate southward directed transport of detritus from low metamorphic sedimentary and magmatic source areas into an Upper Devonian nonvolcanic basin. © Ferdinand Enke Verlag Stuttgart 1985
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title_short	Palaeozoic flysch series in the Coastal Cordillera of Northern Chile
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Palaeozoic flysch series in the Coastal Cordillera of Northern Chile

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