Dolomite Mountains and the origin of the dolomite rock of which they mainly consist: historical developments and new perspectives

@article{Mckenzie2009DolomiteMA,
  title={Dolomite Mountains and the origin of the dolomite rock of which they mainly consist: historical developments and new perspectives},
  author={Judith A. Mckenzie and Cris{\'o}gono Vasconcelos},
  journal={Sedimentology},
  year={2009},
  volume={56}
}
Beginning in the late 18th Century, the Dolomite Mountains in Northern Italy have been the location for major sedimentological developments, from the discovery of the mineral dolomite to the formulation of the coral‐reef hypothesis to explain the origin of the massive dolomite structures that define the splendid scenery of the region. Further, the Dolomite Mountains have inspired voluminous research into the origin of dolomite, questioning whether dolomite is a primary precipitate or a… 
Dolomite formation in the shallow seas of the Alpine Triassic
The Alpine Triassic units of Switzerland, Northern Italy and Western Austria offer an extensive geological archive, in which the enigmatic process of dolomite formation can be studied in a
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A NEW MODEL FOR THE FORMATION OF DOLOMITE IN THE TRIASSIC DOLOMITES, NORTHERN ITALY
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DOLOMITES WITHIN THE MESOZOIC CARBONATES OF SORRENTO PENINSULA (SOUTHERN APENNINES - ITALY): GENETIC MODELS AND RESERVOIR IMPLICATIONS
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Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the “dolomite problem”
TLDR
Constraints on the formation of massive dolomicrite deposits of the Ediacaran Doushantuo Formation are placed, suggesting that the preponderance of dolomite in Paleozoic and Precambrian deposits likely reflects oceanic conditions specific to those eras and that dolostones can be faithful recorders of environmental conditions in the early oceans.
Nucleation and stabilization of Eocene dolomite in evaporative lacustrine deposits from central Tibetan plateau
In past decades, the formation of dolomite at low temperature has been widely studied in both natural systems and cultured experiments, yet the mechanism(s) involved in the nucleation and
Biancone transformed into dolosparite: evidence for secondary recrystallisation (Dolomite Mountains, S.Tyrol, N.Italy)
Information is provided about the dolosparite from the Puez area (Gardenacia Plateau, Southern Alps) near Wolkenstein (S.Tyrol, N.Italy). At the Puez locality on the northern part of the Trento
An Early Holocene Primary Dolomite Layer of Abiotic Origin in Lake Sayram, Central Asia
The “dolomite problem” is a long‐standing puzzle in sedimentology and mineralogy. Previous studies have shown that some dolostones are formed by microbes or in hydrothermal–burial environments. Here,
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