The North-Chilean Coast Range — an example for the development of an active continental margin

Abstract Analysis of extended plutons in the Coast Range of North Chile between 25°30′ and 26°35′ led to the recognition of a complex magmatic and structural evolution from the Upper Paleozoic to the Tertiary. The ascension of the intrusive bodies is dictated by deep-seated block tectonics. Generall...
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Gespeichert in:

Autor*in:	Berg, Karsten [verfasserIn] Breitkreuz, Christoph Damm, Klaus -Werner Pichowiak, Siegfried Zeil, Werner

Format:	Artikel
Sprache:	Englisch

Erschienen:	1983

Schlagwörter:	Structural Geology Orogen Continental Margin Structural Evolution Active Continental Margin

Anmerkung:	© Ferdinand Enke Verlag Stuttgart 1983

Übergeordnetes Werk:	Enthalten in: Geologische Rundschau - Springer-Verlag, 1910, 72(1983), 2 vom: Juni, Seite 715-731
Übergeordnetes Werk:	volume:72 ; year:1983 ; number:2 ; month:06 ; pages:715-731

Links:	Volltext

DOI / URN:	10.1007/BF01822090

Katalog-ID:	OLC2070402940

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520			\|a Abstract Analysis of extended plutons in the Coast Range of North Chile between 25°30′ and 26°35′ led to the recognition of a complex magmatic and structural evolution from the Upper Paleozoic to the Tertiary. The ascension of the intrusive bodies is dictated by deep-seated block tectonics. Generally the chemistry changes from S-type magmas in the Paleozoic to I-type magmas in the Mesozoic and Cainozoic. This is accompanied by a change in the structural geology of the continental margin which we present in six hypothetic phases (Devonian-Tertiary). We are only at the beginning of an encompassing synthesis of the genesis of the Andean orogen.
650		4	\|a Structural Geology
650		4	\|a Orogen
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650		4	\|a Structural Evolution
650		4	\|a Active Continental Margin
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allfields	10.1007/BF01822090 doi (DE-627)OLC2070402940 (DE-He213)BF01822090-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Berg, Karsten verfasserin aut The North-Chilean Coast Range — an example for the development of an active continental margin 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1983 Abstract Analysis of extended plutons in the Coast Range of North Chile between 25°30′ and 26°35′ led to the recognition of a complex magmatic and structural evolution from the Upper Paleozoic to the Tertiary. The ascension of the intrusive bodies is dictated by deep-seated block tectonics. Generally the chemistry changes from S-type magmas in the Paleozoic to I-type magmas in the Mesozoic and Cainozoic. This is accompanied by a change in the structural geology of the continental margin which we present in six hypothetic phases (Devonian-Tertiary). We are only at the beginning of an encompassing synthesis of the genesis of the Andean orogen. Structural Geology Orogen Continental Margin Structural Evolution Active Continental Margin Breitkreuz, Christoph aut Damm, Klaus -Werner aut Pichowiak, Siegfried aut Zeil, Werner aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 72(1983), 2 vom: Juni, Seite 715-731 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:72 year:1983 number:2 month:06 pages:715-731 https://doi.org/10.1007/BF01822090 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_39 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 72 1983 2 06 715-731
spelling	10.1007/BF01822090 doi (DE-627)OLC2070402940 (DE-He213)BF01822090-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Berg, Karsten verfasserin aut The North-Chilean Coast Range — an example for the development of an active continental margin 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1983 Abstract Analysis of extended plutons in the Coast Range of North Chile between 25°30′ and 26°35′ led to the recognition of a complex magmatic and structural evolution from the Upper Paleozoic to the Tertiary. The ascension of the intrusive bodies is dictated by deep-seated block tectonics. Generally the chemistry changes from S-type magmas in the Paleozoic to I-type magmas in the Mesozoic and Cainozoic. This is accompanied by a change in the structural geology of the continental margin which we present in six hypothetic phases (Devonian-Tertiary). We are only at the beginning of an encompassing synthesis of the genesis of the Andean orogen. Structural Geology Orogen Continental Margin Structural Evolution Active Continental Margin Breitkreuz, Christoph aut Damm, Klaus -Werner aut Pichowiak, Siegfried aut Zeil, Werner aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 72(1983), 2 vom: Juni, Seite 715-731 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:72 year:1983 number:2 month:06 pages:715-731 https://doi.org/10.1007/BF01822090 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_39 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 72 1983 2 06 715-731
allfields_unstemmed	10.1007/BF01822090 doi (DE-627)OLC2070402940 (DE-He213)BF01822090-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Berg, Karsten verfasserin aut The North-Chilean Coast Range — an example for the development of an active continental margin 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1983 Abstract Analysis of extended plutons in the Coast Range of North Chile between 25°30′ and 26°35′ led to the recognition of a complex magmatic and structural evolution from the Upper Paleozoic to the Tertiary. The ascension of the intrusive bodies is dictated by deep-seated block tectonics. Generally the chemistry changes from S-type magmas in the Paleozoic to I-type magmas in the Mesozoic and Cainozoic. This is accompanied by a change in the structural geology of the continental margin which we present in six hypothetic phases (Devonian-Tertiary). We are only at the beginning of an encompassing synthesis of the genesis of the Andean orogen. Structural Geology Orogen Continental Margin Structural Evolution Active Continental Margin Breitkreuz, Christoph aut Damm, Klaus -Werner aut Pichowiak, Siegfried aut Zeil, Werner aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 72(1983), 2 vom: Juni, Seite 715-731 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:72 year:1983 number:2 month:06 pages:715-731 https://doi.org/10.1007/BF01822090 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_39 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 72 1983 2 06 715-731
allfieldsGer	10.1007/BF01822090 doi (DE-627)OLC2070402940 (DE-He213)BF01822090-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Berg, Karsten verfasserin aut The North-Chilean Coast Range — an example for the development of an active continental margin 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1983 Abstract Analysis of extended plutons in the Coast Range of North Chile between 25°30′ and 26°35′ led to the recognition of a complex magmatic and structural evolution from the Upper Paleozoic to the Tertiary. The ascension of the intrusive bodies is dictated by deep-seated block tectonics. Generally the chemistry changes from S-type magmas in the Paleozoic to I-type magmas in the Mesozoic and Cainozoic. This is accompanied by a change in the structural geology of the continental margin which we present in six hypothetic phases (Devonian-Tertiary). We are only at the beginning of an encompassing synthesis of the genesis of the Andean orogen. Structural Geology Orogen Continental Margin Structural Evolution Active Continental Margin Breitkreuz, Christoph aut Damm, Klaus -Werner aut Pichowiak, Siegfried aut Zeil, Werner aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 72(1983), 2 vom: Juni, Seite 715-731 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:72 year:1983 number:2 month:06 pages:715-731 https://doi.org/10.1007/BF01822090 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_39 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 72 1983 2 06 715-731
allfieldsSound	10.1007/BF01822090 doi (DE-627)OLC2070402940 (DE-He213)BF01822090-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Berg, Karsten verfasserin aut The North-Chilean Coast Range — an example for the development of an active continental margin 1983 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1983 Abstract Analysis of extended plutons in the Coast Range of North Chile between 25°30′ and 26°35′ led to the recognition of a complex magmatic and structural evolution from the Upper Paleozoic to the Tertiary. The ascension of the intrusive bodies is dictated by deep-seated block tectonics. Generally the chemistry changes from S-type magmas in the Paleozoic to I-type magmas in the Mesozoic and Cainozoic. This is accompanied by a change in the structural geology of the continental margin which we present in six hypothetic phases (Devonian-Tertiary). We are only at the beginning of an encompassing synthesis of the genesis of the Andean orogen. Structural Geology Orogen Continental Margin Structural Evolution Active Continental Margin Breitkreuz, Christoph aut Damm, Klaus -Werner aut Pichowiak, Siegfried aut Zeil, Werner aut Enthalten in Geologische Rundschau Springer-Verlag, 1910 72(1983), 2 vom: Juni, Seite 715-731 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:72 year:1983 number:2 month:06 pages:715-731 https://doi.org/10.1007/BF01822090 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_39 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 72 1983 2 06 715-731
language	English
source	Enthalten in Geologische Rundschau 72(1983), 2 vom: Juni, Seite 715-731 volume:72 year:1983 number:2 month:06 pages:715-731
sourceStr	Enthalten in Geologische Rundschau 72(1983), 2 vom: Juni, Seite 715-731 volume:72 year:1983 number:2 month:06 pages:715-731
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Structural Geology Orogen Continental Margin Structural Evolution Active Continental Margin
dewey-raw	550
isfreeaccess_bool	false
container_title	Geologische Rundschau
authorswithroles_txt_mv	Berg, Karsten @@aut@@ Breitkreuz, Christoph @@aut@@ Damm, Klaus -Werner @@aut@@ Pichowiak, Siegfried @@aut@@ Zeil, Werner @@aut@@
publishDateDaySort_date	1983-06-01T00:00:00Z
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author	Berg, Karsten
spellingShingle	Berg, Karsten ddc 550 ssgn 13 misc Structural Geology misc Orogen misc Continental Margin misc Structural Evolution misc Active Continental Margin The North-Chilean Coast Range — an example for the development of an active continental margin
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topic_title	550 VZ 13 ssgn The North-Chilean Coast Range — an example for the development of an active continental margin Structural Geology Orogen Continental Margin Structural Evolution Active Continental Margin
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title_full	The North-Chilean Coast Range — an example for the development of an active continental margin
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title_sort	the north-chilean coast range — an example for the development of an active continental margin
title_auth	The North-Chilean Coast Range — an example for the development of an active continental margin
abstract	Abstract Analysis of extended plutons in the Coast Range of North Chile between 25°30′ and 26°35′ led to the recognition of a complex magmatic and structural evolution from the Upper Paleozoic to the Tertiary. The ascension of the intrusive bodies is dictated by deep-seated block tectonics. Generally the chemistry changes from S-type magmas in the Paleozoic to I-type magmas in the Mesozoic and Cainozoic. This is accompanied by a change in the structural geology of the continental margin which we present in six hypothetic phases (Devonian-Tertiary). We are only at the beginning of an encompassing synthesis of the genesis of the Andean orogen. © Ferdinand Enke Verlag Stuttgart 1983
abstractGer	Abstract Analysis of extended plutons in the Coast Range of North Chile between 25°30′ and 26°35′ led to the recognition of a complex magmatic and structural evolution from the Upper Paleozoic to the Tertiary. The ascension of the intrusive bodies is dictated by deep-seated block tectonics. Generally the chemistry changes from S-type magmas in the Paleozoic to I-type magmas in the Mesozoic and Cainozoic. This is accompanied by a change in the structural geology of the continental margin which we present in six hypothetic phases (Devonian-Tertiary). We are only at the beginning of an encompassing synthesis of the genesis of the Andean orogen. © Ferdinand Enke Verlag Stuttgart 1983
abstract_unstemmed	Abstract Analysis of extended plutons in the Coast Range of North Chile between 25°30′ and 26°35′ led to the recognition of a complex magmatic and structural evolution from the Upper Paleozoic to the Tertiary. The ascension of the intrusive bodies is dictated by deep-seated block tectonics. Generally the chemistry changes from S-type magmas in the Paleozoic to I-type magmas in the Mesozoic and Cainozoic. This is accompanied by a change in the structural geology of the continental margin which we present in six hypothetic phases (Devonian-Tertiary). We are only at the beginning of an encompassing synthesis of the genesis of the Andean orogen. © Ferdinand Enke Verlag Stuttgart 1983
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title_short	The North-Chilean Coast Range — an example for the development of an active continental margin
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The North-Chilean Coast Range — an example for the development of an active continental margin

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