Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin

Abstract Zircon and apatite fission-track analyses from Late Carboniferous felsic volcanic rocks of the NE German Basin (Halle area and Friedland drilling) reveal at least two major post-emplacement thermal events. After initial cooling at ca. 300 Ma, the volcanic pile underwent a major thermal even...
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Autor*in:	Jacobs, Joachim [verfasserIn] Breitkreuz, Christoph

Format:	Artikel
Sprache:	Englisch

Erschienen:	2003

Schlagwörter:	Fission-track analysis NE German Basin Late Palaeozoic (sub-)volcanic rocks Thermochronology Zircon

Anmerkung:	© Springer-Verlag 2003

Übergeordnetes Werk:	Enthalten in: International journal of earth sciences - Springer-Verlag, 1999, 92(2003), 2 vom: 09. Apr., Seite 165-172
Übergeordnetes Werk:	volume:92 ; year:2003 ; number:2 ; day:09 ; month:04 ; pages:165-172

Links:	Volltext

DOI / URN:	10.1007/s00531-003-0314-2

Katalog-ID:	OLC2070415929

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allfields	10.1007/s00531-003-0314-2 doi (DE-627)OLC2070415929 (DE-He213)s00531-003-0314-2-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Jacobs, Joachim verfasserin aut Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2003 Abstract Zircon and apatite fission-track analyses from Late Carboniferous felsic volcanic rocks of the NE German Basin (Halle area and Friedland drilling) reveal at least two major post-emplacement thermal events. After initial cooling at ca. 300 Ma, the volcanic pile underwent a major thermal event at ca. 200 Ma that reached in most places ca. 250–280 °C and led to the new growth of clay minerals. This event is recorded in the zircon fission-track data and can be related to Jurassic–Triassic rifting in Europe. Another thermal event is recorded in the apatite samples at ca. 100 Ma. A close correlation is observed between apatite fission-track age, texture, and sample alteration. Coarse-grained samples are stronger altered and have younger fission-track ages. Hydrothermal alteration coupled with advective heating probably caused these Upper Cretaceous fission-track ages. The latter event can be related to block faulting and inversion of the European plate during the early stages of the Alpine orogeny. Fission-track analysis NE German Basin Late Palaeozoic (sub-)volcanic rocks Thermochronology Zircon Breitkreuz, Christoph aut Enthalten in International journal of earth sciences Springer-Verlag, 1999 92(2003), 2 vom: 09. Apr., Seite 165-172 (DE-627)270428879 (DE-600)1477582-7 (DE-576)078189780 1437-3254 nnns volume:92 year:2003 number:2 day:09 month:04 pages:165-172 https://doi.org/10.1007/s00531-003-0314-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_24 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_154 GBV_ILN_183 GBV_ILN_188 GBV_ILN_267 GBV_ILN_381 GBV_ILN_600 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_2346 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4320 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 92 2003 2 09 04 165-172
spelling	10.1007/s00531-003-0314-2 doi (DE-627)OLC2070415929 (DE-He213)s00531-003-0314-2-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Jacobs, Joachim verfasserin aut Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2003 Abstract Zircon and apatite fission-track analyses from Late Carboniferous felsic volcanic rocks of the NE German Basin (Halle area and Friedland drilling) reveal at least two major post-emplacement thermal events. After initial cooling at ca. 300 Ma, the volcanic pile underwent a major thermal event at ca. 200 Ma that reached in most places ca. 250–280 °C and led to the new growth of clay minerals. This event is recorded in the zircon fission-track data and can be related to Jurassic–Triassic rifting in Europe. Another thermal event is recorded in the apatite samples at ca. 100 Ma. A close correlation is observed between apatite fission-track age, texture, and sample alteration. Coarse-grained samples are stronger altered and have younger fission-track ages. Hydrothermal alteration coupled with advective heating probably caused these Upper Cretaceous fission-track ages. The latter event can be related to block faulting and inversion of the European plate during the early stages of the Alpine orogeny. Fission-track analysis NE German Basin Late Palaeozoic (sub-)volcanic rocks Thermochronology Zircon Breitkreuz, Christoph aut Enthalten in International journal of earth sciences Springer-Verlag, 1999 92(2003), 2 vom: 09. Apr., Seite 165-172 (DE-627)270428879 (DE-600)1477582-7 (DE-576)078189780 1437-3254 nnns volume:92 year:2003 number:2 day:09 month:04 pages:165-172 https://doi.org/10.1007/s00531-003-0314-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_24 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_154 GBV_ILN_183 GBV_ILN_188 GBV_ILN_267 GBV_ILN_381 GBV_ILN_600 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_2346 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4320 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 92 2003 2 09 04 165-172
allfields_unstemmed	10.1007/s00531-003-0314-2 doi (DE-627)OLC2070415929 (DE-He213)s00531-003-0314-2-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Jacobs, Joachim verfasserin aut Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2003 Abstract Zircon and apatite fission-track analyses from Late Carboniferous felsic volcanic rocks of the NE German Basin (Halle area and Friedland drilling) reveal at least two major post-emplacement thermal events. After initial cooling at ca. 300 Ma, the volcanic pile underwent a major thermal event at ca. 200 Ma that reached in most places ca. 250–280 °C and led to the new growth of clay minerals. This event is recorded in the zircon fission-track data and can be related to Jurassic–Triassic rifting in Europe. Another thermal event is recorded in the apatite samples at ca. 100 Ma. A close correlation is observed between apatite fission-track age, texture, and sample alteration. Coarse-grained samples are stronger altered and have younger fission-track ages. Hydrothermal alteration coupled with advective heating probably caused these Upper Cretaceous fission-track ages. The latter event can be related to block faulting and inversion of the European plate during the early stages of the Alpine orogeny. Fission-track analysis NE German Basin Late Palaeozoic (sub-)volcanic rocks Thermochronology Zircon Breitkreuz, Christoph aut Enthalten in International journal of earth sciences Springer-Verlag, 1999 92(2003), 2 vom: 09. Apr., Seite 165-172 (DE-627)270428879 (DE-600)1477582-7 (DE-576)078189780 1437-3254 nnns volume:92 year:2003 number:2 day:09 month:04 pages:165-172 https://doi.org/10.1007/s00531-003-0314-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_24 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_154 GBV_ILN_183 GBV_ILN_188 GBV_ILN_267 GBV_ILN_381 GBV_ILN_600 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_2346 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4320 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 92 2003 2 09 04 165-172
allfieldsGer	10.1007/s00531-003-0314-2 doi (DE-627)OLC2070415929 (DE-He213)s00531-003-0314-2-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Jacobs, Joachim verfasserin aut Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2003 Abstract Zircon and apatite fission-track analyses from Late Carboniferous felsic volcanic rocks of the NE German Basin (Halle area and Friedland drilling) reveal at least two major post-emplacement thermal events. After initial cooling at ca. 300 Ma, the volcanic pile underwent a major thermal event at ca. 200 Ma that reached in most places ca. 250–280 °C and led to the new growth of clay minerals. This event is recorded in the zircon fission-track data and can be related to Jurassic–Triassic rifting in Europe. Another thermal event is recorded in the apatite samples at ca. 100 Ma. A close correlation is observed between apatite fission-track age, texture, and sample alteration. Coarse-grained samples are stronger altered and have younger fission-track ages. Hydrothermal alteration coupled with advective heating probably caused these Upper Cretaceous fission-track ages. The latter event can be related to block faulting and inversion of the European plate during the early stages of the Alpine orogeny. Fission-track analysis NE German Basin Late Palaeozoic (sub-)volcanic rocks Thermochronology Zircon Breitkreuz, Christoph aut Enthalten in International journal of earth sciences Springer-Verlag, 1999 92(2003), 2 vom: 09. Apr., Seite 165-172 (DE-627)270428879 (DE-600)1477582-7 (DE-576)078189780 1437-3254 nnns volume:92 year:2003 number:2 day:09 month:04 pages:165-172 https://doi.org/10.1007/s00531-003-0314-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_24 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_154 GBV_ILN_183 GBV_ILN_188 GBV_ILN_267 GBV_ILN_381 GBV_ILN_600 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_2346 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4320 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 92 2003 2 09 04 165-172
allfieldsSound	10.1007/s00531-003-0314-2 doi (DE-627)OLC2070415929 (DE-He213)s00531-003-0314-2-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Jacobs, Joachim verfasserin aut Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2003 Abstract Zircon and apatite fission-track analyses from Late Carboniferous felsic volcanic rocks of the NE German Basin (Halle area and Friedland drilling) reveal at least two major post-emplacement thermal events. After initial cooling at ca. 300 Ma, the volcanic pile underwent a major thermal event at ca. 200 Ma that reached in most places ca. 250–280 °C and led to the new growth of clay minerals. This event is recorded in the zircon fission-track data and can be related to Jurassic–Triassic rifting in Europe. Another thermal event is recorded in the apatite samples at ca. 100 Ma. A close correlation is observed between apatite fission-track age, texture, and sample alteration. Coarse-grained samples are stronger altered and have younger fission-track ages. Hydrothermal alteration coupled with advective heating probably caused these Upper Cretaceous fission-track ages. The latter event can be related to block faulting and inversion of the European plate during the early stages of the Alpine orogeny. Fission-track analysis NE German Basin Late Palaeozoic (sub-)volcanic rocks Thermochronology Zircon Breitkreuz, Christoph aut Enthalten in International journal of earth sciences Springer-Verlag, 1999 92(2003), 2 vom: 09. Apr., Seite 165-172 (DE-627)270428879 (DE-600)1477582-7 (DE-576)078189780 1437-3254 nnns volume:92 year:2003 number:2 day:09 month:04 pages:165-172 https://doi.org/10.1007/s00531-003-0314-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_24 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_154 GBV_ILN_183 GBV_ILN_188 GBV_ILN_267 GBV_ILN_381 GBV_ILN_600 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_2346 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4320 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 AR 92 2003 2 09 04 165-172
language	English
source	Enthalten in International journal of earth sciences 92(2003), 2 vom: 09. Apr., Seite 165-172 volume:92 year:2003 number:2 day:09 month:04 pages:165-172
sourceStr	Enthalten in International journal of earth sciences 92(2003), 2 vom: 09. Apr., Seite 165-172 volume:92 year:2003 number:2 day:09 month:04 pages:165-172
format_phy_str_mv	Article
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topic_facet	Fission-track analysis NE German Basin Late Palaeozoic (sub-)volcanic rocks Thermochronology Zircon
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isfreeaccess_bool	false
container_title	International journal of earth sciences
authorswithroles_txt_mv	Jacobs, Joachim @@aut@@ Breitkreuz, Christoph @@aut@@
publishDateDaySort_date	2003-04-09T00:00:00Z
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author	Jacobs, Joachim
spellingShingle	Jacobs, Joachim ddc 550 ssgn 13 misc Fission-track analysis misc NE German Basin misc Late Palaeozoic (sub-)volcanic rocks misc Thermochronology misc Zircon Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin
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title	Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin
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title_full	Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin
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title_sort	zircon and apatite fission-track thermochronology of late carboniferous volcanic rocks of the ne german basin
title_auth	Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin
abstract	Abstract Zircon and apatite fission-track analyses from Late Carboniferous felsic volcanic rocks of the NE German Basin (Halle area and Friedland drilling) reveal at least two major post-emplacement thermal events. After initial cooling at ca. 300 Ma, the volcanic pile underwent a major thermal event at ca. 200 Ma that reached in most places ca. 250–280 °C and led to the new growth of clay minerals. This event is recorded in the zircon fission-track data and can be related to Jurassic–Triassic rifting in Europe. Another thermal event is recorded in the apatite samples at ca. 100 Ma. A close correlation is observed between apatite fission-track age, texture, and sample alteration. Coarse-grained samples are stronger altered and have younger fission-track ages. Hydrothermal alteration coupled with advective heating probably caused these Upper Cretaceous fission-track ages. The latter event can be related to block faulting and inversion of the European plate during the early stages of the Alpine orogeny. © Springer-Verlag 2003
abstractGer	Abstract Zircon and apatite fission-track analyses from Late Carboniferous felsic volcanic rocks of the NE German Basin (Halle area and Friedland drilling) reveal at least two major post-emplacement thermal events. After initial cooling at ca. 300 Ma, the volcanic pile underwent a major thermal event at ca. 200 Ma that reached in most places ca. 250–280 °C and led to the new growth of clay minerals. This event is recorded in the zircon fission-track data and can be related to Jurassic–Triassic rifting in Europe. Another thermal event is recorded in the apatite samples at ca. 100 Ma. A close correlation is observed between apatite fission-track age, texture, and sample alteration. Coarse-grained samples are stronger altered and have younger fission-track ages. Hydrothermal alteration coupled with advective heating probably caused these Upper Cretaceous fission-track ages. The latter event can be related to block faulting and inversion of the European plate during the early stages of the Alpine orogeny. © Springer-Verlag 2003
abstract_unstemmed	Abstract Zircon and apatite fission-track analyses from Late Carboniferous felsic volcanic rocks of the NE German Basin (Halle area and Friedland drilling) reveal at least two major post-emplacement thermal events. After initial cooling at ca. 300 Ma, the volcanic pile underwent a major thermal event at ca. 200 Ma that reached in most places ca. 250–280 °C and led to the new growth of clay minerals. This event is recorded in the zircon fission-track data and can be related to Jurassic–Triassic rifting in Europe. Another thermal event is recorded in the apatite samples at ca. 100 Ma. A close correlation is observed between apatite fission-track age, texture, and sample alteration. Coarse-grained samples are stronger altered and have younger fission-track ages. Hydrothermal alteration coupled with advective heating probably caused these Upper Cretaceous fission-track ages. The latter event can be related to block faulting and inversion of the European plate during the early stages of the Alpine orogeny. © Springer-Verlag 2003
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title_short	Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin
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Zircon and apatite fission-track thermochronology of Late Carboniferous volcanic rocks of the NE German Basin

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