التفاصيل البيبلوغرافية
| العنوان: |
Hints on the late miocene evolution of the Tonale-Adamello-Brenta Region (Alps, Italy) based on allochtonous sediments from Raponzolo Cave |
| المؤلفون: |
Sauro, Francesco, Fellin, Maria Giuditta, Columbu, Andrea, Haeuselmann, Philipp, Borsato, Andrea, Carbone, Cristina, De Waele, Jo De |
| المساهمون: |
The University of Newcastle. College of Engineering, Science & Environment, School of Environmental and Life Sciences |
| بيانات النشر: |
Frontiers Research Foundation |
| سنة النشر: |
2021 |
| المجموعة: |
NOVA: The University of Newcastle Research Online (Australia) |
| مصطلحات موضوعية: |
Al-Be isotopes, speleogenesis, paleogeography, cave sediments, AFT analysis, U-Pb zircon dating |
| الوصف: |
Raponzolo is a paleo-phreatic cave explored in 2011 in the Brenta Dolomites (Trentino, Italy), at the remarkable altitude of 2,560 m a.s.l. Differently to all other caves of the area, it hosts well-cemented fine to medium sands of granitic-metamorphic composition. The composition suggests a sediment source from the Adamello and Tonale Unit, separated from the Brenta by one of the most important tectonic lineaments of the Alps (Giudicarie Line). The fine-sand sediment was sampled to determine burial time and thus a minimum age of the cave. Cosmogenic isotopes ( 26 Al and 10 Be) in quartz grains allowed to estimate a minimum burial age of 5.25 Ma based on the mean sediment transport time at the surface and infer original altitude of the catchment area. Detrital apatite fission-track (AFT) and U-Pb dating on zircons provide information on the source, both from a regional and altitude (exhumation) perspective. Two populations of detrital AFT ages center at 17 (−2.3 + 2.6) Ma and 23 (−3.3 + 3.9) Ma, whereas the main detrital zircon U-Pb age populations are younger than 40 Ma. These correspond to intrusive and metamorphic sources nowadays outcropping exclusively above 2,200–2,300 m a.s.l. in Northern Adamello and Tonale. The results point to a late Miocene erosion and infilling of the cave by allochtonous sediments, with important implications on the timing of cave speleogenesis, as well as the paleogeographical connection, tectonic evolution and uplift of different structural units of the Alps. The roundness and the well sorted size of the quartz grains suggest a fluvial or aeolian origin, possibly recycled by glacial activity related to cold events reported in high latitude areas of the world at 5.75 and 5.51 Ma. These glacial phases have never been documented before in the Alps. This information confirms that the valleys dividing these geological units were not yet deeply entrenched during the onset of the Messinian Salinity Crisis (5.6–5.5 Ma), allowing an efficient transport of sediments across major tectonic ... |
| نوع الوثيقة: |
article in journal/newspaper |
| اللغة: |
English |
| Relation: |
Frontiers in Earth Science Vol. 9, no. 672119; http://hdl.handle.net/1959.13/1458594; uon:45464 |
| الاتاحة: |
http://hdl.handle.net/1959.13/1458594 |
| Rights: |
© 2021 Sauro, Fellin, Columbu, Häuselmann, Borsato, Carbone and De Waele. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. |
| رقم الانضمام: |
edsbas.26C84313 |
| قاعدة البيانات: |
BASE |