Authigenic and detrital clay minerals as indicators of paleoenvironmental and postdepositional evolution in a Cretaceous–Cenozoic succession from Argentine Central Andes

Author:

Wunderlin Cecilia A.,Collo Gilda,Ezpeleta Miguel,Reinoso Carbonell Virginia V.,Nóbile Julieta C.,Ciccioli Patricia L.,Faudone Sonia

Funder

Consejo Nacional de Investigaciones Científicas y Técnicas

Agencia Nacional de Promoción Científica y Tecnológica

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference86 articles.

1. Very low-grade hydrothermal metamorphism of basic igneous rocks;Alt,1999

2. Mio–Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods;Amidon;Proceedings of the National Academy of Sciences of the United States of America,2017

3. Effect of aqueous Si/Mg ratio and pH on the nucleation and growth of sepiolite at 25 °C;Baldermann;Geochimica et Cosmochimica Acta,2018

4. Early kaolinization of detrital Weald facies in the Galve Sub-basin (Central Iberian Chain, north-east Spain) and its relationship to paleoclimate;Bauluz;Cretaceous Research,2014

5. Chlorite and chloritization processes through mixed-layer mineral series in low-temperature geological systems – a review;Beaufort;Clay Minerals,2015

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