Camille Paquez - Academia.edu (original) (raw)

Papers by Camille Paquez

Research paper thumbnail of U-Pb, 40Ar/39Ar, (U-Th)/He, and zircon double-dating geochronology of Intrusive and Explosive Activity on Piton des Neiges Volcano, Réunion Island

This dataset contains seven tables related to the publication "Multi-technique Geochronology... more This dataset contains seven tables related to the publication "Multi-technique Geochronology of Intrusive and Explosive Activity on Piton des Neiges Volcano, Réunion Island". Tables 1 to 4 present the data related to the main text of the article, while Tables S1 to S3 present the data related to the Supplementary Information of this publication. Table 1 contains U-Pb data on zircons from intrusive and explosive rocks. Table 2 contains 40Ar/39Ar data on phlogopites from intrusive rocks. Table 3 contains (U-Th)/He data on zircons and apatites from intrusive and explosive rocks. Table 4 contains zircon double-dating data from tephras. Table S1 summarizes the Cameca SIMS settings. Table S2 presents the U-Th data used for zircon double-dating on tephras (Cameca SIMS). Table S3 contains the U-Pb data used for zircon double-dating on tephra sample RN18-9 (Cameca SIMS).

Research paper thumbnail of Moving Disabled People into the Workforce

Research paper thumbnail of Multi‐technique Geochronology of Intrusive and Explosive Activity on Piton des Neiges Volcano, Réunion Island

Geochemistry, Geophysics, Geosystems, 2022

Research paper thumbnail of Co-Ni-arsenide mineralisation in the Bou Azzer district (Anti-Atlas, Morocco): Genetic model and tectonic implications

Research paper thumbnail of How do cirques form in ocean island volcanoes: the case of Piton des Neiges (Réunion Island, Indian Ocean)

<p&amp... more <p>“Cirques” are funnel-shaped, seaward-narrowing valleys commonly observed on many volcanic islands worldwide, such as Tahiti (French Polynesia), La Palma or Gran Canaria (Canary), Anjouan (Comores), and Maui or Molokai (Hawai’i). Because they contradict the basics of regressive erosion by rivers, these geomorphic structures have been interpreted in many ways, including the erosion of volcano-tectonic depressions (crater, caldera, rift zone), the formation of leaf grabens caused by volcano spreading, or the subsidence of dense plutonic bodies within edifices. Piton des Neiges volcano (Réunion Island) is dissected by three cirques (Salazie, Mafate and Cilaos) and thus provides an excellent case to study the processes that lead to the formation of these funnel-shaped valleys. To do so, we performed a detailed field and photogrammetric mapping of the volcanic and volcaniclastic products outcropping in the cirques using an updated chrono-stratigraphy.</p> <p>Our mapping reveals that the three cirques of Piton des Neiges are not delimited by faults, which excludes vertical movements as the primary cause of their formation. Rather, the cirques are built on former horseshoe-shaped depressions filled with volcaniclastic breccias (mostly related to debris avalanches and debris flows), and later covered by lava flow units. Importantly, the breccia are several hundred meters thick in the innermost parts of the cirques, but thin out until complete disappearance toward the outer flanks of the volcano.</p> <p>In consequence, we interpret the basal volcaniclastic breccias as playing a major role in the formation of the cirques, by offering a weaker resistance than the lava flow units. This contrasted resistance leads to greater erosion rates on the inside of the volcano than on the outer flanks and, hence explaining the reverted funnel shape of the cirques. In our model, cirques are therefore erosional structures mostly guided by past dismantling episodes rather than by tectonic or volcano-tectonic structures.</p>

Research paper thumbnail of U-Pb, 40Ar/39Ar, (U-Th)/He, and zircon double-dating geochronology of Intrusive and Explosive Activity on Piton des Neiges Volcano, Réunion Island

This dataset contains seven tables related to the publication "Multi-technique Geochronology... more This dataset contains seven tables related to the publication "Multi-technique Geochronology of Intrusive and Explosive Activity on Piton des Neiges Volcano, Réunion Island". Tables 1 to 4 present the data related to the main text of the article, while Tables S1 to S3 present the data related to the Supplementary Information of this publication. Table 1 contains U-Pb data on zircons from intrusive and explosive rocks. Table 2 contains 40Ar/39Ar data on phlogopites from intrusive rocks. Table 3 contains (U-Th)/He data on zircons and apatites from intrusive and explosive rocks. Table 4 contains zircon double-dating data from tephras. Table S1 summarizes the Cameca SIMS settings. Table S2 presents the U-Th data used for zircon double-dating on tephras (Cameca SIMS). Table S3 contains the U-Pb data used for zircon double-dating on tephra sample RN18-9 (Cameca SIMS).

Research paper thumbnail of Moving Disabled People into the Workforce

Research paper thumbnail of Multi‐technique Geochronology of Intrusive and Explosive Activity on Piton des Neiges Volcano, Réunion Island

Geochemistry, Geophysics, Geosystems, 2022

Research paper thumbnail of Co-Ni-arsenide mineralisation in the Bou Azzer district (Anti-Atlas, Morocco): Genetic model and tectonic implications

Research paper thumbnail of How do cirques form in ocean island volcanoes: the case of Piton des Neiges (Réunion Island, Indian Ocean)

<p&amp... more <p>“Cirques” are funnel-shaped, seaward-narrowing valleys commonly observed on many volcanic islands worldwide, such as Tahiti (French Polynesia), La Palma or Gran Canaria (Canary), Anjouan (Comores), and Maui or Molokai (Hawai’i). Because they contradict the basics of regressive erosion by rivers, these geomorphic structures have been interpreted in many ways, including the erosion of volcano-tectonic depressions (crater, caldera, rift zone), the formation of leaf grabens caused by volcano spreading, or the subsidence of dense plutonic bodies within edifices. Piton des Neiges volcano (Réunion Island) is dissected by three cirques (Salazie, Mafate and Cilaos) and thus provides an excellent case to study the processes that lead to the formation of these funnel-shaped valleys. To do so, we performed a detailed field and photogrammetric mapping of the volcanic and volcaniclastic products outcropping in the cirques using an updated chrono-stratigraphy.</p> <p>Our mapping reveals that the three cirques of Piton des Neiges are not delimited by faults, which excludes vertical movements as the primary cause of their formation. Rather, the cirques are built on former horseshoe-shaped depressions filled with volcaniclastic breccias (mostly related to debris avalanches and debris flows), and later covered by lava flow units. Importantly, the breccia are several hundred meters thick in the innermost parts of the cirques, but thin out until complete disappearance toward the outer flanks of the volcano.</p> <p>In consequence, we interpret the basal volcaniclastic breccias as playing a major role in the formation of the cirques, by offering a weaker resistance than the lava flow units. This contrasted resistance leads to greater erosion rates on the inside of the volcano than on the outer flanks and, hence explaining the reverted funnel shape of the cirques. In our model, cirques are therefore erosional structures mostly guided by past dismantling episodes rather than by tectonic or volcano-tectonic structures.</p>