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Tohru Ohta

Researcher at Waseda University

Publications -  32
Citations -  676

Tohru Ohta is an academic researcher from Waseda University. The author has contributed to research in topics: Sedimentary depositional environment & Geology. The author has an hindex of 11, co-authored 28 publications receiving 511 citations.

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Statistical empirical index of chemical weathering in igneous rocks: A new tool for evaluating the degree of weathering

TL;DR: In this article, an alternative statistical empirical index of chemical weathering that is extracted by the principal component analysis (PCA) of a large dataset derived from unweathered igneous rocks and their weathering profiles is presented.
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Geochemistry of Jurassic to earliest Cretaceous deposits in the Nagato Basin, SW Japan: implication of factor analysis to sorting effects and provenance signatures

TL;DR: In this article, the authors used factor analysis to address geochemical responses to the sorting effect and provenance of Late Mesozoic sediments in the Nagato Basin, SW Japan.
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Measuring and adjusting the weathering and hydraulic sorting effects for rigorous provenance analysis of sedimentary rocks: a case study from the Jurassic Ashikita Group, south‐west Japan

TL;DR: In this paper, two geochemical diagrams for provenance analysis were utilized, which incorporate full consideration of compositional modifications resulting from weathering (MFW diagram) and hydraulic sorting processes (SiO2/Al2O3-Na2O/K2O diagram).
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Paleoclimatic conditions and paleoweathering processes on Mesozoic continental redbeds from Western-Central Mediterranean Alpine Chains

TL;DR: In this paper, chemical and mineral analyses of the Triassic to lowermost Jurassic mudstones from continental redbeds outcropping in the Internal Domains of the Betic-Rifian and Calabria-Peloritani chains have been used to infer the relationships between paleoclimatic conditions and paleoweathering processes during rifting of a continental crust block that finally detached from adjoining western Tethyan realms to form an independent microplate (Mesomediterranean Microplate) from Jurassic to lower Miocene time.