Geochemistry, geochronology and petrogenesis of Maya Block granitoids and dykes from the Chicxulub Impact Crater, Gulf of México: Implications for the assembly of Pangea

@article{Zhao2020GeochemistryGA,
  title={Geochemistry, geochronology and petrogenesis of Maya Block granitoids and dykes from the Chicxulub Impact Crater, Gulf of M{\'e}xico: Implications for the assembly of Pangea},
  author={Jiawei Zhao and Long Xiao and Sean P. S. Gulick and Joanna V. Morgan and David A. Kring and Jaime Urrutia Fucugauchi and Martin Schmieder and Sietze J. de Graaff and Axel Wittmann and Catherine H. Ross and Philippe Claeys and Annemarie E. Pickersgill and Pim Kaskes and Steven Goderis and Cornelia Rasmussen and Vivi Vajda and Ludovic Ferri{\`e}re and Jean‐Guillaume Feignon and Elise Chenot and Ligia P{\'e}rez‐Cruz and Honami Sato and Kosei E. Yamaguchi},
  journal={Gondwana Research},
  year={2020}
}

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References

SHOWING 1-10 OF 231 REFERENCES

Study of melt and a clast of 546 Ma magmatic arc rocks in the 65 Ma Chicxulub bolide breccia, northern Maya block, Mexico: western limit of Ediacaran arc peripheral to northern Gondwana

The basement of the Maya block of eastern Mexico is generally covered by Mesozoic and Cenozoic platformal carbonate rocks. However, the 65.5 Ma Chicxulub meteorite impact in the northern Yucatan

Geochemical variability of the Yucatàn basement: Constraints from crystalline clasts in Chicxulub impactites

Abstract— The 65 Ma old Chicxulub impact structure with a diameter of about 180 km is again in the focus of the geosciences because of the recently commenced drilling of the scientific well

Geochemistry of Mississippian tuffs from the Ouachita Mountains, and implications for the tectonics of the Ouachita orogen, Oklahoma and Arkansas

The Ouachita orogeny was the result of plate convergence at the southern margin of the North American continent, although the nature of the converging southern plate and the direction of subduction

The Tuzancoa Formation: Evidence of an Early Permian Submarine Continental Arc in East-Central Mexico

Paleozoic rocks exposed in northeast Hidalgo State, Mexico, have traditionally been assigned to the Guacamaya Formation, a orogenic flysch assemblage associated with the collision of South and North

Chicxulub impactites: Geochemical clues to the precursor rocks

Abstract— The 65 Ma Chicxulub impact structure, Mexico, with a diameter of ∼180 km is the focus of geoscientific research because of its link to the mass extinction event at the Cretaceous‐Tertiary

Late Paleozoic collision, delamination, short-lived magmatism, and rapid denudation in the Meguma Terrane (Nova Scotia, Canada): constraints from 40Ar/39Ar isotopic data

The Meguma Terrane consists of 8–15 km of early Paleozoic stratified rocks, deposited on a continental basement, that were deformed and metamorphosed during the late Paleozoic as a result of
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