What is he best known for?
The fields of study he is best known for:
- Oceanography
- Paleontology
- Sedimentary rock
Theodore C. Moore mainly focuses on Paleontology, Oceanography, Cenozoic, Paleoclimatology and Radiolaria.
His study focuses on the intersection of Paleontology and fields such as Isotopes of oxygen with connections in the field of Series, Benthic zone and Interglacial.
His Oceanography research is multidisciplinary, relying on both Meltwater, Glacial period and Water level.
Theodore C. Moore works mostly in the field of Cenozoic, limiting it down to topics relating to Paleoceanography and, in certain cases, Pacific ocean, Drilling, Deep sea, Circumpolar deep water and Marine geology, as a part of the same area of interest.
His Chronostratigraphy research incorporates elements of Hydrology, Geodesy, Chronology and 100,000-year problem.
His studies in Ice age integrate themes in fields like Marine isotope stage and Stratigraphy.
His most cited work include:
- Age dating and the orbital theory of the ice ages: Development of a high-resolution 0 to 300,000-year chronostratigraphy (2919 citations)
- The Cenozoic palaeoenvironment of the Arctic Ocean. (411 citations)
- Cenozoic history and paleoceanography of the central equatorial Pacific Ocean: A regional synthesis of Deep Sea Drilling Project data (365 citations)
What are the main themes of his work throughout his whole career to date?
His main research concerns Paleontology, Oceanography, Cenozoic, Sediment and Paleogene.
Paleontology and Drilling are commonly linked in his work.
Isotopes of oxygen is closely connected to Glacial period in his research, which is encompassed under the umbrella topic of Oceanography.
His research integrates issues of Deep sea, Basement, Paleoceanography and Carbonate compensation depth in his study of Cenozoic.
The study incorporates disciplines such as Latitude and Crust in addition to Sediment.
His Paleogene study integrates concerns from other disciplines, such as Pacific Plate, Paleomagnetism and Equator.
He most often published in these fields:
- Paleontology (46.56%)
- Oceanography (37.04%)
- Cenozoic (18.52%)
What were the highlights of his more recent work (between 2009-2019)?
- Paleontology (46.56%)
- Oceanography (37.04%)
- Table (6.88%)
In recent papers he was focusing on the following fields of study:
His main research concerns Paleontology, Oceanography, Table, Mineralogy and Drilling.
His Paleontology study frequently links to adjacent areas such as Isotopes of oxygen.
Many of his studies on Oceanography involve topics that are commonly interrelated, such as Pleistocene.
His Table research is multidisciplinary, incorporating elements of Hydrology, Combinatorics and Latitude, Geodesy.
His Drilling research is multidisciplinary, relying on both Sedimentary rock and Cenozoic.
His Cenozoic study combines topics from a wide range of disciplines, such as Deep sea, Transect, Pacific Rim and Paleogene.
Between 2009 and 2019, his most popular works were:
- A Cenozoic record of the equatorial Pacific carbonate compensation depth (208 citations)
- Direct stratigraphic dating of India-Asia collision onset at the Selandian (middle Paleocene, 59 ± 1 Ma) (206 citations)
- Revised composite depth scales and integration of IODP Sites U1331-U1334 and ODP Sites 1218-1220 (34 citations)
In his most recent research, the most cited papers focused on:
- Oceanography
- Paleontology
- Sedimentary rock
His scientific interests lie mostly in Oceanography, Paleontology, Cenozoic, Paleogene and Paleoclimatology.
His Oceanography study incorporates themes from Sedimentary depositional environment and Pleistocene.
His Paleontology study frequently links to related topics such as Isotopes of oxygen.
Theodore C. Moore studied Cenozoic and Drilling that intersect with Pacific Rim, Deep sea, Paleomagnetism, Stratigraphy and Transect.
His Paleogene research incorporates elements of Sedimentary rock, Geochemistry, Weathering, Calcium carbonate and Carbon dioxide in Earth's atmosphere.
His studies deal with areas such as Low latitude, Pacific ocean, Chronostratigraphy and Radiolaria as well as Biostratigraphy.
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