What is he best known for?
The fields of study he is best known for:
- Sedimentary rock
- Paleontology
- Geochemistry
His scientific interests lie mostly in Stalagmite, Geochemistry, Mineralogy, Calcite and Cave.
Detlev K. Richter focuses mostly in the field of Stalagmite, narrowing it down to matters related to Speleothem and, in some cases, Stalactite, Aquifer, Hydrology and Infiltration.
His research combines Feldspar and Geochemistry.
Detlev K. Richter works in the field of Mineralogy, namely Diagenesis.
His Calcite research incorporates themes from Analytical chemistry and Kinetic fractionation.
His Cave research incorporates elements of North Atlantic oscillation, Thermohaline circulation, Holocene and Clastic rock.
His most cited work include:
- Progress in application of cathodoluminescence (CL) in sedimentary petrology (169 citations)
- Magnesium-isotope fractionation during low-Mg calcite precipitation in a limestone cave – Field study and experiments (127 citations)
- A paleoclimate record of the last 17,600 years in stalagmites from the B7 cave, Sauerland, Germany (93 citations)
What are the main themes of his work throughout his whole career to date?
Detlev K. Richter mainly focuses on Geochemistry, Calcite, Mineralogy, Cave and Stalagmite.
His Geochemistry study frequently involves adjacent topics like Siliciclastic.
His Calcite study integrates concerns from other disciplines, such as Speleothem, Clay minerals, Cement and Cretaceous.
His work deals with themes such as Metamorphic rock, Sedimentary rock, Trace element, Cathodoluminescence and Isotopes of oxygen, which intersect with Mineralogy.
His Cave study incorporates themes from Hydrology, Karst, Permafrost and δ18O.
His research on Holocene and Paleontology is centered around Stalagmite.
He most often published in these fields:
- Geochemistry (37.50%)
- Calcite (36.61%)
- Mineralogy (36.61%)
What were the highlights of his more recent work (between 2014-2020)?
- Calcite (36.61%)
- Mineralogy (36.61%)
- Stalagmite (25.00%)
In recent papers he was focusing on the following fields of study:
The scientist’s investigation covers issues in Calcite, Mineralogy, Stalagmite, Cave and Geochemistry.
His study in the fields of Aragonite under the domain of Calcite overlaps with other disciplines such as Precipitation.
His Mineralogy research incorporates elements of Speleothem, Trace element and Cement.
Detlev K. Richter interconnects Dendrochronology, Isotopes of oxygen and Photochemistry in the investigation of issues within Stalagmite.
His Cave study integrates concerns from other disciplines, such as Hydrology and δ18O.
His work is connected to Dolomite and Diagenesis, as a part of Geochemistry.
Between 2014 and 2020, his most popular works were:
- The magnesium isotope (δ26Mg) signature of dolomites (83 citations)
- Reorganization of the North Atlantic Oscillation during early Holocene deglaciation (64 citations)
- Magnesium isotope composition of sabkha porewater and related (Sub-)Recent stoichiometric dolomites, Abu Dhabi (UAE) (42 citations)
In his most recent research, the most cited papers focused on:
- Sedimentary rock
- Paleontology
- Cretaceous
Detlev K. Richter focuses on Mineralogy, Diagenesis, Geochemistry, Calcite and Dolomite.
His work is dedicated to discovering how Diagenesis, Petrography are connected with Fluid inclusions and Sedimentary depositional environment and other disciplines.
He is interested in Aragonite, which is a field of Geochemistry.
His research integrates issues of Trace element, Stalagmite and Cretaceous in his study of Calcite.
His work focuses on many connections between Dolomite and other disciplines, such as Sabkha, that overlap with his field of interest in Geologic record, Isotopes of magnesium, Seawater and Isotope fractionation.
His work deals with themes such as Speleothem, Cave and North Atlantic oscillation, which intersect with δ18O.
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