Saved in:
Bibliographic Details
Main Authors: Galelli, Claudio, Caccianiga, Lorenzo, Apollonio, Lorenzo, Magnani, Paolo, Breton, Vincent
Format: Preprint
Published: 2025
Subjects:
Online Access:https://arxiv.org/abs/2510.23126
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1866917265647075328
author Galelli, Claudio
Caccianiga, Lorenzo
Apollonio, Lorenzo
Magnani, Paolo
Breton, Vincent
author_facet Galelli, Claudio
Caccianiga, Lorenzo
Apollonio, Lorenzo
Magnani, Paolo
Breton, Vincent
contents We present a phenomenological study demonstrating the feasibility of using olivine xenoliths from the Chaîne des Puys as a time-resolved paleo-detector array to probe the cosmic-ray flux over the last 40,000 years. This volcanic region provides a unique chronosequence of samples brought to the surface by well-dated eruptions. By modeling the expected density of nuclear recoil tracks induced by cosmic-ray muons in olivine, we show that the signal is detectable and above backgrounds from natural radioactivity. We demonstrate that by analyzing samples with different exposure ages, it is possible to construct a time-differential measurement of the cosmic-ray flux. This method shows sensitivity to historical variations, such as the enhanced flux expected during the Laschamp geomagnetic excursion ($\sim$41~kyr) and the potential contribution from nearby supernovae, for which we use the Antlia supernova remnant precursor as a benchmark. This work establishes a new application of the paleo-detector technique for long-scale time-domain high-energy astrophysics and provides the direct scientific motivation for experimental efforts to measure these track records.
format Preprint
id arxiv_https___arxiv_org_abs_2510_23126
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle A volcanic chronosequence as a time-resolved paleo-detector array to study the cosmic-ray flux in the Late Pleistocene and Holocene
Galelli, Claudio
Caccianiga, Lorenzo
Apollonio, Lorenzo
Magnani, Paolo
Breton, Vincent
High Energy Astrophysical Phenomena
High Energy Physics - Phenomenology
We present a phenomenological study demonstrating the feasibility of using olivine xenoliths from the Chaîne des Puys as a time-resolved paleo-detector array to probe the cosmic-ray flux over the last 40,000 years. This volcanic region provides a unique chronosequence of samples brought to the surface by well-dated eruptions. By modeling the expected density of nuclear recoil tracks induced by cosmic-ray muons in olivine, we show that the signal is detectable and above backgrounds from natural radioactivity. We demonstrate that by analyzing samples with different exposure ages, it is possible to construct a time-differential measurement of the cosmic-ray flux. This method shows sensitivity to historical variations, such as the enhanced flux expected during the Laschamp geomagnetic excursion ($\sim$41~kyr) and the potential contribution from nearby supernovae, for which we use the Antlia supernova remnant precursor as a benchmark. This work establishes a new application of the paleo-detector technique for long-scale time-domain high-energy astrophysics and provides the direct scientific motivation for experimental efforts to measure these track records.
title A volcanic chronosequence as a time-resolved paleo-detector array to study the cosmic-ray flux in the Late Pleistocene and Holocene
topic High Energy Astrophysical Phenomena
High Energy Physics - Phenomenology
url https://arxiv.org/abs/2510.23126