The carbonates of the post-Variscan basins of Sardinia: the evolution from Carboniferous–Permian humid-persistent to Permian arid-ephemeral lakes in a morphotectonic framework

Autor: Luca Giacomo Costamagna

Publikováno v: Geological Magazine. 156:1892-1914

Late to post-Variscan sedimentary basins of Sardinia were influenced during Pennsylvanian to Permian times by two main tectono-sedimentary cycles: a Pennsylvanian to Cisuralian cycle represented mainly by dark limnic deposits, overlain by a Guadalupi

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::abc7ac96ac56c83cb498d939bb211371
https://doi.org/10.1017/s0016756819000232

The Atlas-East Variscan -Elbe shear system and its role in the formation of the pull-apart Late Palaeozoic basins

Autor: Laura Gaggero, Federico Mantovani, Franco Marco Elter, Luca Giacomo Costamagna, Enrico Pandeli

Publikováno v: International journal of earth sciences (1999, Internet) 109 (2020): 739–760. doi:10.1007/s00531-020-01830-y
info:cnr-pdr/source/autori:Elter F.M.[1], Gaggero L.[1], Mantovani F.[1], Pandeli E.[2,3], Costamagna L.G.[4]/titolo:The Atlas-East Variscan-Elbe shear system and its role in the formation of the pull-apart Late Palaeozoic basins/doi:10.1007%2Fs00531-020-01830-y/rivista:International journal of earth sciences (1999, Internet)/anno:2020/pagina_da:739/pagina_a:760/intervallo_pagine:739–760/volume:109

The Variscan orogeny occurred as a result of the Late Devonian to Late Carboniferous collision and accretion of Gondwana-derived microcontinents and continental masses with those of Laurussia. The irregular boundaries of the colliding continents caus

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::402aa0fac243d2398ebae3577d96edfc
https://publications.cnr.it/doc/458941

Evolution of a Pyrenean molassic basin in the Western Mediterranean area: The Eocene-Oligocene Cixerri Formation in Southern Sardinia (Italy)

Autor: Luca Giacomo Costamagna, Andreas Schäfer

Publikováno v: Geological Journal. 53:424-437

The sedimentary features of the Cixerri Formation (Eocene–Oligocene) and its evolution in space and time are described through mapping, investigation of all the significant outcrops, and also by analysing the depositional architecture of well-expos

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::b6d22bee617c00e0c4fada2294922c17
https://doi.org/10.1002/gj.2911

Middle Jurassic continental to marine transition in an extensional tectonics context: the Genna Selole Fm depositional system in the Tacchi area (central Sardinia, Italy)

Autor: Luca Giacomo Costamagna

Publikováno v: Geological Journal. 51:722-736

In Eastern Sardinia during the early Middle Jurassic, Alpine Tethys opening triggered the rise of a temporary tectonic high. The high collapsed rapidly, was fragmented into separate blocks, and subsequently covered by continental, transitional, and f

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::7e68860adaab81bffea029e8163b630b
https://doi.org/10.1002/gj.2680

The Middle Jurassic Alpine Tethyan Unconformity and the Eastern Sardinia - Corsica Jurassic High: A sedimentary and regional analysis

Autor: Luca Giacomo Costamagna

Publikováno v: Journal of Iberian Geology. 42

Investigations performed along the Middle Jurassic Alpine Tethyan unconformity surface of E Sardinia evidenced an elaborate surface that developed over older Late Paleozoic to Triassic rocks. This surface is covered by the Middle Jurassic Genna Selol

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d53dfc0dc3bff2ff163723039d1dbe49
https://doi.org/10.5209/jige.51885