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Sujoy Mukhopadhyay

Researcher at University of California, Davis

Publications -  83
Citations -  4236

Sujoy Mukhopadhyay is an academic researcher from University of California, Davis. The author has contributed to research in topics: Mantle (geology) & Mantle plume. The author has an hindex of 33, co-authored 78 publications receiving 3734 citations. Previous affiliations of Sujoy Mukhopadhyay include California Institute of Technology & Carnegie Institution for Science.

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Isotopic Compositions of Cometary Matter Returned by Stardust

TL;DR: Hydrogen, carbon, nitrogen, and oxygen isotopic compositions are heterogeneous among comet 81P/Wild 2 particle fragments; however, extreme isotopic anomalies are rare, indicating that the comet is not a pristine aggregate of presolar materials.
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Early differentiation and volatile accretion recorded in deep-mantle neon and xenon

TL;DR: New noble gas measurements from an Icelandic OIB reveal differences in elemental abundances and 20Ne/22Ne ratios between the Iceland mantle plume and the MORB source, showing that Earth’s mantle accreted volatiles from at least two separate sources and that neither the Moon-forming impact nor 4.45 billion years of mantle convection has erased the signature of Earth's heterogeneous accretion and early differentiation.
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Interstellar chemistry recorded in organic matter from primitive meteorites

TL;DR: It is shown that hydrogen and nitrogen isotopic compositions in carbonaceous chondrite organic matter reach and even exceed those found in interplanetary dust particles, preserving primitive organics that were a component of the original building blocks of the solar system.
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Preservation of Earth-forming events in the tungsten isotopic composition of modern flood basalts.

TL;DR: High-precision tungsten isotopic data from rocks from two large igneous provinces, the North Atlantic Igneous Province and the Ontong Java Plateau, reveal preservation to the Phanerozoic of tung sten isotopic heterogeneities in the mantle, indicating that portions of the mantle that formed during Earth's primary accretionary period have survived to the present.