His primary scientific interests are in Mineralogy, Hot spring, Calcite, Geochemistry and Paleontology. Brian Jones combines subjects such as Geyserite, Cementation and Sedimentary rock with his study of Mineralogy. The various areas that he examines in his Hot spring study include Volcano, Ecology, Spring, Stromatolite and Subaerial.
His Calcite research includes elements of Crystal growth, Crystal, Cement and Holocene climatic optimum. His Geochemistry study combines topics in areas such as Tufa and Rift valley. His Paleontology research is multidisciplinary, incorporating elements of Reef, Fringing reef, Benthic zone and Sea level.
Brian Jones mainly focuses on Paleontology, Mineralogy, Calcite, Geochemistry and Diagenesis. His Paleontology research integrates issues from Reef, Oceanography, Sea level and Arctic. His research integrates issues of Geyserite, Hot spring, Crystal and Spring in his study of Mineralogy.
His biological study deals with issues like Cave, which deal with fields such as Karst. In his research, Facies is intimately related to Sedimentary depositional environment, which falls under the overarching field of Geochemistry. His Diagenesis study which covers Pleistocene that intersects with Quaternary.
Brian Jones mainly investigates Geochemistry, Paleontology, Diagenesis, Calcite and Dolomitization. His work deals with themes such as Piedra, Spring and Facies, which intersect with Geochemistry. His Structural basin, Neogene and Tectonics study in the realm of Paleontology connects with subjects such as Cayman Islands.
The Diagenesis study combines topics in areas such as Quaternary and Meteoric water. Calcite is a subfield of Mineralogy that Brian Jones studies. The study incorporates disciplines such as Sea level, Dolostone and Dolomite in addition to Dolomitization.
Brian Jones spends much of his time researching Calcite, Geochemistry, Mineralogy, Aragonite and Dolomitization. The study of Calcite is intertwined with the study of Sedimentary depositional environment in a number of ways. His research on Sedimentary depositional environment concerns the broader Paleontology.
Brian Jones undertakes interdisciplinary study in the fields of Geochemistry and Microbial mat through his research. His Aragonite research includes themes of Nanocrystal, Crystal and Spring. His Dolomitization study combines topics from a wide range of disciplines, such as Dolomite, Diagenesis, Tectonic subsidence, Sea level and Neogene.
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Geochemistry of brachiopods: Oxygen and carbon isotopic records of Paleozoic oceans☆
Ján Veizer;Peter Fritz;Brian Jones.
Geochimica et Cosmochimica Acta (1986)
Nutrient-Gradient Controls on Devonian Reefs: Insight from the Ramp-Situated Alexandra Reef System (Frasnian), Northwest Territories, Canada
Alex J. MacNeil;Brian Jones.
Special Publication - Society for Sedimentary Geology (2008)
Absolute depths of Silurian benthic assemblages
Carlton E. Brett;Arthur J. Boucot;Brian Jones.
Lethaia (1993)
Biogenicity of Silica Precipitation Around Geysers and Hot-Spring Vents, North Island, New Zealand
Brian Jones;Robin W. Renaut;Michael R. Rosen.
Journal of Sedimentary Research (1997)
Microbial Biofacies in Hot-Spring Sinters: A Model Based on Ohaaki Pool, North Island, New Zealand
Brian Jones;Robin W. Renaut;Michael R. Rosen.
Journal of Sedimentary Research (1998)
Origin of Carbonate Sedimentary Rocks
Noel P. James;Brian Jones.
(2015)
Rapid in situ silicification of microbes at Loburu hot springs, Lake Bogoria, Kenya Rift Valley
R. W. Renaut;B. Jones;J.‐J. Tiercelin.
Sedimentology (1998)
Anatomy of a fringing reef around Grand Cayman; storm rubble, not coral framework
Paul Blanchon;Brian Jones;William Kalbfleisch.
Journal of Sedimentary Research (1997)
Calcite Moonmilk: Crystal Morphology and Environment of Formation in Caves in the Italian Alps
Andrea Borsato;Silvia Frisia;Brian Jones;Klaas Van Der Borg.
Journal of Sedimentary Research (2000)
The microbial role in hot spring silicification.
Kurt O. Konhauser;Brian Jones;Vernon R. Phoenix;Grant Ferris.
AMBIO: A Journal of the Human Environment (2004)
Sedimentary Geology
(Impact Factor: 3.329)
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