Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France

Abstract A three-point Sm–Nd isotope isochron on fluorite from the very large Montroc fluorite vein deposit (southern Massif Central, France) defines an age of 111±13 Ma. Initial $ ε_{Nd} $ of −8.6 and initial 87Sr/86Sr of ~0.71245 suggest an upper crustal source of the hydrothermal system, in agree...
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Autor*in:	Munoz, Marguerite [verfasserIn] Premo, Wayne R. Courjault-Radé, Pierre

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2004

Schlagwörter:	Sm–Nd isotopic analyses Isochron age Fluorite Cretaceous Montroc France

Anmerkung:	© Springer-Verlag 2004

Übergeordnetes Werk:	Enthalten in: Mineralium deposita - Berlin : Springer, 1966, 39(2004), 8 vom: 14. Dez., Seite 970-975
Übergeordnetes Werk:	volume:39 ; year:2004 ; number:8 ; day:14 ; month:12 ; pages:970-975

Links:	Volltext

DOI / URN:	10.1007/s00126-004-0453-9

Katalog-ID:	SPR001024647

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520			\|a Abstract A three-point Sm–Nd isotope isochron on fluorite from the very large Montroc fluorite vein deposit (southern Massif Central, France) defines an age of 111±13 Ma. Initial $ ε_{Nd} $ of −8.6 and initial 87Sr/86Sr of ~0.71245 suggest an upper crustal source of the hydrothermal system, in agreement with earlier work on fluid inclusions which indicated a basinal brine origin. The mid-Cretaceous age of ~111 Ma suggests the Albian/Aptian transition as the most likely period for large-scale fluid circulation during a regional extensional tectonic event, related to the opening of the North Atlantic ocean.
650		4	\|a Sm–Nd isotopic analyses \|7 (dpeaa)DE-He213
650		4	\|a Isochron age \|7 (dpeaa)DE-He213
650		4	\|a Fluorite \|7 (dpeaa)DE-He213
650		4	\|a Cretaceous \|7 (dpeaa)DE-He213
650		4	\|a Montroc \|7 (dpeaa)DE-He213
650		4	\|a France \|7 (dpeaa)DE-He213
700	1		\|a Premo, Wayne R. \|4 aut
700	1		\|a Courjault-Radé, Pierre \|4 aut
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publishDate	2004
allfields	10.1007/s00126-004-0453-9 doi (DE-627)SPR001024647 (SPR)s00126-004-0453-9-e DE-627 ger DE-627 rakwb eng Munoz, Marguerite verfasserin aut Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2004 Abstract A three-point Sm–Nd isotope isochron on fluorite from the very large Montroc fluorite vein deposit (southern Massif Central, France) defines an age of 111±13 Ma. Initial $ ε_{Nd} $ of −8.6 and initial 87Sr/86Sr of ~0.71245 suggest an upper crustal source of the hydrothermal system, in agreement with earlier work on fluid inclusions which indicated a basinal brine origin. The mid-Cretaceous age of ~111 Ma suggests the Albian/Aptian transition as the most likely period for large-scale fluid circulation during a regional extensional tectonic event, related to the opening of the North Atlantic ocean. Sm–Nd isotopic analyses (dpeaa)DE-He213 Isochron age (dpeaa)DE-He213 Fluorite (dpeaa)DE-He213 Cretaceous (dpeaa)DE-He213 Montroc (dpeaa)DE-He213 France (dpeaa)DE-He213 Premo, Wayne R. aut Courjault-Radé, Pierre aut Enthalten in Mineralium deposita Berlin : Springer, 1966 39(2004), 8 vom: 14. Dez., Seite 970-975 (DE-627)254630014 (DE-600)1462046-7 1432-1866 nnns volume:39 year:2004 number:8 day:14 month:12 pages:970-975 https://dx.doi.org/10.1007/s00126-004-0453-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 39 2004 8 14 12 970-975
spelling	10.1007/s00126-004-0453-9 doi (DE-627)SPR001024647 (SPR)s00126-004-0453-9-e DE-627 ger DE-627 rakwb eng Munoz, Marguerite verfasserin aut Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2004 Abstract A three-point Sm–Nd isotope isochron on fluorite from the very large Montroc fluorite vein deposit (southern Massif Central, France) defines an age of 111±13 Ma. Initial $ ε_{Nd} $ of −8.6 and initial 87Sr/86Sr of ~0.71245 suggest an upper crustal source of the hydrothermal system, in agreement with earlier work on fluid inclusions which indicated a basinal brine origin. The mid-Cretaceous age of ~111 Ma suggests the Albian/Aptian transition as the most likely period for large-scale fluid circulation during a regional extensional tectonic event, related to the opening of the North Atlantic ocean. Sm–Nd isotopic analyses (dpeaa)DE-He213 Isochron age (dpeaa)DE-He213 Fluorite (dpeaa)DE-He213 Cretaceous (dpeaa)DE-He213 Montroc (dpeaa)DE-He213 France (dpeaa)DE-He213 Premo, Wayne R. aut Courjault-Radé, Pierre aut Enthalten in Mineralium deposita Berlin : Springer, 1966 39(2004), 8 vom: 14. Dez., Seite 970-975 (DE-627)254630014 (DE-600)1462046-7 1432-1866 nnns volume:39 year:2004 number:8 day:14 month:12 pages:970-975 https://dx.doi.org/10.1007/s00126-004-0453-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 39 2004 8 14 12 970-975
allfields_unstemmed	10.1007/s00126-004-0453-9 doi (DE-627)SPR001024647 (SPR)s00126-004-0453-9-e DE-627 ger DE-627 rakwb eng Munoz, Marguerite verfasserin aut Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2004 Abstract A three-point Sm–Nd isotope isochron on fluorite from the very large Montroc fluorite vein deposit (southern Massif Central, France) defines an age of 111±13 Ma. Initial $ ε_{Nd} $ of −8.6 and initial 87Sr/86Sr of ~0.71245 suggest an upper crustal source of the hydrothermal system, in agreement with earlier work on fluid inclusions which indicated a basinal brine origin. The mid-Cretaceous age of ~111 Ma suggests the Albian/Aptian transition as the most likely period for large-scale fluid circulation during a regional extensional tectonic event, related to the opening of the North Atlantic ocean. Sm–Nd isotopic analyses (dpeaa)DE-He213 Isochron age (dpeaa)DE-He213 Fluorite (dpeaa)DE-He213 Cretaceous (dpeaa)DE-He213 Montroc (dpeaa)DE-He213 France (dpeaa)DE-He213 Premo, Wayne R. aut Courjault-Radé, Pierre aut Enthalten in Mineralium deposita Berlin : Springer, 1966 39(2004), 8 vom: 14. Dez., Seite 970-975 (DE-627)254630014 (DE-600)1462046-7 1432-1866 nnns volume:39 year:2004 number:8 day:14 month:12 pages:970-975 https://dx.doi.org/10.1007/s00126-004-0453-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 39 2004 8 14 12 970-975
allfieldsGer	10.1007/s00126-004-0453-9 doi (DE-627)SPR001024647 (SPR)s00126-004-0453-9-e DE-627 ger DE-627 rakwb eng Munoz, Marguerite verfasserin aut Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2004 Abstract A three-point Sm–Nd isotope isochron on fluorite from the very large Montroc fluorite vein deposit (southern Massif Central, France) defines an age of 111±13 Ma. Initial $ ε_{Nd} $ of −8.6 and initial 87Sr/86Sr of ~0.71245 suggest an upper crustal source of the hydrothermal system, in agreement with earlier work on fluid inclusions which indicated a basinal brine origin. The mid-Cretaceous age of ~111 Ma suggests the Albian/Aptian transition as the most likely period for large-scale fluid circulation during a regional extensional tectonic event, related to the opening of the North Atlantic ocean. Sm–Nd isotopic analyses (dpeaa)DE-He213 Isochron age (dpeaa)DE-He213 Fluorite (dpeaa)DE-He213 Cretaceous (dpeaa)DE-He213 Montroc (dpeaa)DE-He213 France (dpeaa)DE-He213 Premo, Wayne R. aut Courjault-Radé, Pierre aut Enthalten in Mineralium deposita Berlin : Springer, 1966 39(2004), 8 vom: 14. Dez., Seite 970-975 (DE-627)254630014 (DE-600)1462046-7 1432-1866 nnns volume:39 year:2004 number:8 day:14 month:12 pages:970-975 https://dx.doi.org/10.1007/s00126-004-0453-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 39 2004 8 14 12 970-975
allfieldsSound	10.1007/s00126-004-0453-9 doi (DE-627)SPR001024647 (SPR)s00126-004-0453-9-e DE-627 ger DE-627 rakwb eng Munoz, Marguerite verfasserin aut Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France 2004 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2004 Abstract A three-point Sm–Nd isotope isochron on fluorite from the very large Montroc fluorite vein deposit (southern Massif Central, France) defines an age of 111±13 Ma. Initial $ ε_{Nd} $ of −8.6 and initial 87Sr/86Sr of ~0.71245 suggest an upper crustal source of the hydrothermal system, in agreement with earlier work on fluid inclusions which indicated a basinal brine origin. The mid-Cretaceous age of ~111 Ma suggests the Albian/Aptian transition as the most likely period for large-scale fluid circulation during a regional extensional tectonic event, related to the opening of the North Atlantic ocean. Sm–Nd isotopic analyses (dpeaa)DE-He213 Isochron age (dpeaa)DE-He213 Fluorite (dpeaa)DE-He213 Cretaceous (dpeaa)DE-He213 Montroc (dpeaa)DE-He213 France (dpeaa)DE-He213 Premo, Wayne R. aut Courjault-Radé, Pierre aut Enthalten in Mineralium deposita Berlin : Springer, 1966 39(2004), 8 vom: 14. Dez., Seite 970-975 (DE-627)254630014 (DE-600)1462046-7 1432-1866 nnns volume:39 year:2004 number:8 day:14 month:12 pages:970-975 https://dx.doi.org/10.1007/s00126-004-0453-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 39 2004 8 14 12 970-975
language	English
source	Enthalten in Mineralium deposita 39(2004), 8 vom: 14. Dez., Seite 970-975 volume:39 year:2004 number:8 day:14 month:12 pages:970-975
sourceStr	Enthalten in Mineralium deposita 39(2004), 8 vom: 14. Dez., Seite 970-975 volume:39 year:2004 number:8 day:14 month:12 pages:970-975
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Sm–Nd isotopic analyses Isochron age Fluorite Cretaceous Montroc France
isfreeaccess_bool	false
container_title	Mineralium deposita
authorswithroles_txt_mv	Munoz, Marguerite @@aut@@ Premo, Wayne R. @@aut@@ Courjault-Radé, Pierre @@aut@@
publishDateDaySort_date	2004-12-14T00:00:00Z
hierarchy_top_id	254630014
id	SPR001024647
language_de	englisch
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author	Munoz, Marguerite
spellingShingle	Munoz, Marguerite misc Sm–Nd isotopic analyses misc Isochron age misc Fluorite misc Cretaceous misc Montroc misc France Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France
authorStr	Munoz, Marguerite
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topic_title	Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France Sm–Nd isotopic analyses (dpeaa)DE-He213 Isochron age (dpeaa)DE-He213 Fluorite (dpeaa)DE-He213 Cretaceous (dpeaa)DE-He213 Montroc (dpeaa)DE-He213 France (dpeaa)DE-He213
topic	misc Sm–Nd isotopic analyses misc Isochron age misc Fluorite misc Cretaceous misc Montroc misc France
topic_unstemmed	misc Sm–Nd isotopic analyses misc Isochron age misc Fluorite misc Cretaceous misc Montroc misc France
topic_browse	misc Sm–Nd isotopic analyses misc Isochron age misc Fluorite misc Cretaceous misc Montroc misc France
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title	Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France
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title_full	Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France
author_sort	Munoz, Marguerite
journal	Mineralium deposita
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author_browse	Munoz, Marguerite Premo, Wayne R. Courjault-Radé, Pierre
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author-letter	Munoz, Marguerite
doi_str_mv	10.1007/s00126-004-0453-9
title_sort	sm–nd dating of fluorite from the worldclass montroc fluorite deposit, southern massif central, france
title_auth	Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France
abstract	Abstract A three-point Sm–Nd isotope isochron on fluorite from the very large Montroc fluorite vein deposit (southern Massif Central, France) defines an age of 111±13 Ma. Initial $ ε_{Nd} $ of −8.6 and initial 87Sr/86Sr of ~0.71245 suggest an upper crustal source of the hydrothermal system, in agreement with earlier work on fluid inclusions which indicated a basinal brine origin. The mid-Cretaceous age of ~111 Ma suggests the Albian/Aptian transition as the most likely period for large-scale fluid circulation during a regional extensional tectonic event, related to the opening of the North Atlantic ocean. © Springer-Verlag 2004
abstractGer	Abstract A three-point Sm–Nd isotope isochron on fluorite from the very large Montroc fluorite vein deposit (southern Massif Central, France) defines an age of 111±13 Ma. Initial $ ε_{Nd} $ of −8.6 and initial 87Sr/86Sr of ~0.71245 suggest an upper crustal source of the hydrothermal system, in agreement with earlier work on fluid inclusions which indicated a basinal brine origin. The mid-Cretaceous age of ~111 Ma suggests the Albian/Aptian transition as the most likely period for large-scale fluid circulation during a regional extensional tectonic event, related to the opening of the North Atlantic ocean. © Springer-Verlag 2004
abstract_unstemmed	Abstract A three-point Sm–Nd isotope isochron on fluorite from the very large Montroc fluorite vein deposit (southern Massif Central, France) defines an age of 111±13 Ma. Initial $ ε_{Nd} $ of −8.6 and initial 87Sr/86Sr of ~0.71245 suggest an upper crustal source of the hydrothermal system, in agreement with earlier work on fluid inclusions which indicated a basinal brine origin. The mid-Cretaceous age of ~111 Ma suggests the Albian/Aptian transition as the most likely period for large-scale fluid circulation during a regional extensional tectonic event, related to the opening of the North Atlantic ocean. © Springer-Verlag 2004
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title_short	Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France
url	https://dx.doi.org/10.1007/s00126-004-0453-9
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author2	Premo, Wayne R. Courjault-Radé, Pierre
author2Str	Premo, Wayne R. Courjault-Radé, Pierre
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doi_str	10.1007/s00126-004-0453-9
up_date	2024-07-03T19:49:10.668Z
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Initial $ ε_{Nd} $ of −8.6 and initial 87Sr/86Sr of ~0.71245 suggest an upper crustal source of the hydrothermal system, in agreement with earlier work on fluid inclusions which indicated a basinal brine origin. 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Sm–Nd dating of fluorite from the worldclass Montroc fluorite deposit, southern Massif Central, France

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