Dating tectonic activity in the Lepontine Dome and Rhone-Simplon Fault regions through hydrothermal monazite-(Ce)
<p><strong>Abstract.</strong> Zoned hydrothermal monazite-(Ce) from Alpine-type fissures and clefts is used to gain new insights into the tectonic history of the Lepontine Dome in the Central Alps and the timing of deformation along the Rhone-Simplon Fault zone on the dome's w...
Gespeichert in:
| 1. Verfasser: | |
|---|---|
| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
| Veröffentlicht: |
21 February 2020
|
| In: |
Solid earth
Year: 2020, Jahrgang: 11, Heft: 1, Pages: 199-222 |
| ISSN: | 1869-9529 |
| DOI: | 10.5194/se-11-199-2020 |
| Online-Zugang: | Verlag, lizenzpflichtig, Volltext: https://doi.org/10.5194/se-11-199-2020 Verlag, lizenzpflichtig, Volltext: https://www.solid-earth.net/11/199/2020/ 
|
| Verfasserangaben: | Christian A. Bergemann, Edwin Gnos, Alfons Berger, Emilie Janots, and Martin J. Whitehouse |
MARC
| LEADER | 00000caa a2200000 c 4500 | ||
|---|---|---|---|
| 001 | 1693625199 | ||
| 003 | DE-627 | ||
| 005 | 20220818023514.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 200331s2020 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.5194/se-11-199-2020 |2 doi | |
| 035 | |a (DE-627)1693625199 | ||
| 035 | |a (DE-599)KXP1693625199 | ||
| 035 | |a (OCoLC)1341311624 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rda | ||
| 041 | |a eng | ||
| 084 | |a 31 |2 sdnb | ||
| 100 | 1 | |a Bergemann, Christian A. |e VerfasserIn |0 (DE-588)1207349712 |0 (DE-627)1693624796 |4 aut | |
| 245 | 1 | 0 | |a Dating tectonic activity in the Lepontine Dome and Rhone-Simplon Fault regions through hydrothermal monazite-(Ce) |c Christian A. Bergemann, Edwin Gnos, Alfons Berger, Emilie Janots, and Martin J. Whitehouse |
| 264 | 1 | |c 21 February 2020 | |
| 300 | |a 24 | ||
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a Computermedien |b c |2 rdamedia | ||
| 338 | |a Online-Ressource |b cr |2 rdacarrier | ||
| 500 | |a Gesehen am 31.03.2020 | ||
| 520 | |a <p><strong>Abstract.</strong> Zoned hydrothermal monazite-(Ce) from Alpine-type fissures and clefts is used to gain new insights into the tectonic history of the Lepontine Dome in the Central Alps and the timing of deformation along the Rhone-Simplon Fault zone on the dome's western end. Hydrothermal monazites-(Ce) (re)crystallization ages directly date deformation that induces changes in physicochemical conditions of the fissure or cleft fluid. A total of 480 secondary ion mass spectrometry (SIMS) spot analyses from 20 individual crystals, including co-type material of the monazite-(Nd) type locality, record ages for the time of <span class="inline-formula">∼19</span> to 2.7 <span class="inline-formula">Ma</span>, with individual grains recording age ranges of 2 to 7.5 <span class="inline-formula">Myr</span>. The combination of these age data with geometric considerations and spatial distribution across the Lepontine region gives a more precise young exhumation history for the area. At the northeastern and southwestern edges of the Lepontine Dome, units underwent hydrothermal monazite-(Ce) growth at 19-12.5 and 16.5-10.5 <span class="inline-formula">Ma</span>, respectively, while crystallization of monazite-(Ce) in the eastern Lepontine Dome started later, at 15-10 <span class="inline-formula">Ma</span>. Fissure monazite-(Ce) along the western limit of the dome reports younger ages of 13-7 <span class="inline-formula">Ma</span>. A younger age group around 8-5 <span class="inline-formula">Ma</span> is limited to fissures and clefts associated with the Simplon normal fault and related strike-slip faults such as the Rhone Fault. The data set shows that the monazite-(Ce) age record directly links the fluid-induced interaction between fissure mineral and host rock to the Lepontine Dome's evolution in space and time. A comparison between hydrothermal monazite-(Ce) and thermochronometric data suggest that hydrothermal monazite-(Ce) dating may allow us to identify areas of slow exhumation or cooling rates during ongoing tectonic activity.</p> | ||
| 773 | 0 | 8 | |i Enthalten in |t Solid earth |d Göttingen : Copernicus Publ., 2010 |g 11(2020), 1, Seite 199-222 |h Online-Ressource |w (DE-627)62317720X |w (DE-600)2545676-3 |w (DE-576)321466632 |x 1869-9529 |7 nnas |a Dating tectonic activity in the Lepontine Dome and Rhone-Simplon Fault regions through hydrothermal monazite-(Ce) |
| 773 | 1 | 8 | |g volume:11 |g year:2020 |g number:1 |g pages:199-222 |g extent:24 |a Dating tectonic activity in the Lepontine Dome and Rhone-Simplon Fault regions through hydrothermal monazite-(Ce) |
| 856 | 4 | 0 | |u https://doi.org/10.5194/se-11-199-2020 |x Verlag |x Resolving-System |z lizenzpflichtig |3 Volltext |
| 856 | 4 | 0 | |u https://www.solid-earth.net/11/199/2020/ |x Verlag |z lizenzpflichtig |3 Volltext |
| 951 | |a AR | ||
| 992 | |a 20200331 | ||
| 993 | |a Article | ||
| 994 | |a 2020 | ||
| 998 | |g 1207349712 |a Bergemann, Christian A. |m 1207349712:Bergemann, Christian A. |d 120000 |d 121000 |e 120000PB1207349712 |e 121000PB1207349712 |k 0/120000/ |k 1/120000/121000/ |p 1 |x j | ||
| 999 | |a KXP-PPN1693625199 |e 3616509378 | ||
| BIB | |a Y | ||
| SER | |a journal | ||
| JSO | |a {"title":[{"title_sort":"Dating tectonic activity in the Lepontine Dome and Rhone-Simplon Fault regions through hydrothermal monazite-(Ce)","title":"Dating tectonic activity in the Lepontine Dome and Rhone-Simplon Fault regions through hydrothermal monazite-(Ce)"}],"person":[{"family":"Bergemann","given":"Christian A.","roleDisplay":"VerfasserIn","display":"Bergemann, Christian A.","role":"aut"}],"type":{"media":"Online-Ressource","bibl":"article-journal"},"note":["Gesehen am 31.03.2020"],"recId":"1693625199","language":["eng"],"origin":[{"dateIssuedKey":"2020","dateIssuedDisp":"21 February 2020"}],"id":{"doi":["10.5194/se-11-199-2020"],"eki":["1693625199"]},"name":{"displayForm":["Christian A. Bergemann, Edwin Gnos, Alfons Berger, Emilie Janots, and Martin J. Whitehouse"]},"physDesc":[{"extent":"24 S."}],"relHost":[{"id":{"issn":["1869-9529"],"eki":["62317720X"],"zdb":["2545676-3"]},"origin":[{"dateIssuedKey":"2010","publisher":"Copernicus Publ.","dateIssuedDisp":"2010-","publisherPlace":"Göttingen"}],"physDesc":[{"extent":"Online-Ressource"}],"title":[{"subtitle":"SE ; an interaktive open access journal of the European Geosciences Union","title":"Solid earth","title_sort":"Solid earth"}],"recId":"62317720X","corporate":[{"display":"European Geosciences Union","roleDisplay":"Herausgebendes Organ","role":"isb"}],"language":["eng"],"type":{"media":"Online-Ressource","bibl":"periodical"},"disp":"Dating tectonic activity in the Lepontine Dome and Rhone-Simplon Fault regions through hydrothermal monazite-(Ce)Solid earth","note":["Gesehen am 02.10.20"],"part":{"volume":"11","text":"11(2020), 1, Seite 199-222","extent":"24","year":"2020","pages":"199-222","issue":"1"},"titleAlt":[{"title":"SE"}],"pubHistory":["1.2010 -"]}]} | ||
| SRT | |a BERGEMANNCDATINGTECT2120 | ||