M
Michelangelo Martini
Researcher at National Autonomous University of Mexico
Publications - 40
Citations - 689
Michelangelo Martini is an academic researcher from National Autonomous University of Mexico. The author has contributed to research in topics: Terrane & Cretaceous. The author has an hindex of 12, co-authored 36 publications receiving 520 citations.
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Journal ArticleDOI
Tectono-stratigraphic evolution of eastern Mexico during the break-up of Pangea: A review
TL;DR: The Mesozoic Atlantic System of Mexico can be divided into two tectono-stratigraphic subsystems representing the two main tectonic stages of the break-up of Pangea as mentioned in this paper.
Journal ArticleDOI
Sandstone Provenance of the Arperos Basin (Sierra de Guanajuato, Central Mexico): Late Jurassic-Early Cretaceous Back-Arc Spreading as the Foundation of the Guerrero Terrane
TL;DR: In this paper, a combined study that includes geologic mapping, stratigraphy, U-Pb geochronology, and sandstone provenance data from the Arperos Basin in the Sierra de Guanajuato, central Mexico is presented.
Book ChapterDOI
Cretaceous–Eocene magmatism and Laramide deformation in southwestern Mexico: No role for terrane accretion
Michelangelo Martini,Luca Ferrari,Margarita López-Martínez,Mariano Cerca-Martínez,Victor A. Valencia,Lina Serrano-Durán +5 more
TL;DR: A detailed geologic and structural study and new 40 Ar/39 Ar and U-Pb ages for a broad region in the centraleastern part of the Guerrero terrane that allow the accretion model to be tested is presented in this article.
Journal ArticleDOI
Correlating the Arperos Basin from Guanajuato, central Mexico, to Santo Tomás, southern Mexico: Implications for the paleogeography and origin of the Guerrero terrane
TL;DR: The Guerrero terrane has been interpreted either as a Mesozoic Pacific multi-arc system accreted to North America, or as a detached slice of the North American continental margin, which was rifted during backarc spreading and subsequently accretized back to the continental mainland as mentioned in this paper.
Journal ArticleDOI
Kinematics of the Guerrero terrane accretion in the Sierra de Guanajuato, central Mexico: new insights for the structural evolution of arc–continent collisional zones
TL;DR: The Sierra de Guanajuato is an exposure of the Guerrero terrane suture belt and consists of a complex tectonic pile that formed through at least three major shortening phases: D1SG, D2SG, and D3SG as mentioned in this paper.