Controlling factors and implications for travertine and tufa deposition in a volcanic setting

@article{RodrguezBerriguete2019ControllingFA,
  title={Controlling factors and implications for travertine and tufa deposition in a volcanic setting},
  author={{\'A}lvaro Rodr{\'i}guez-Berriguete and Ana Mar{\'i}a Alonso-Zarza},
  journal={Sedimentary Geology},
  year={2019}
}
Carbonate tufas as archives of climate and sedimentary dynamic in volcanic settings, examples from Gran Canaria (Spain)
Three Holocene tufas from Gran Canaria volcanic island were studied with the aim of deciphering their sedimentary evolution through space and time. Las Temisas tufa (south‐eastern arid part of the
Upper Eocene travertine‐lacustrine carbonate in the Jianchuan basin, southeastern Tibetan Plateau: Reappraisal of its origin and implication for the monsoon climate
The Asian monsoon is one of the largest climatic systems in the world, but age of its onset has been estimated differently ranging from the late Eocene to the Quaternary. We investigated the
Early diagenetic features in Holocene travertine and tufa from a volcanic setting (Azuaje, Gran Canaria, Spain)
The diagenesis of travertine and tufa is rarely considered an issue due to the common difficulty of distinguishing what is primary from secondary, as in most of cases these diagenetic changes occur
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