Michael K. Weisberg mainly focuses on Chondrite, Chondrule, Geochemistry, Meteorite and Mineralogy. The concepts of his Chondrule study are interwoven with issues in Silicate and Olivine. The study incorporates disciplines such as Allende meteorite, Analytical chemistry, Isotopes of oxygen and Forsterite in addition to Olivine.
His work on Lithophile as part of general Geochemistry study is frequently connected to Isotopes of nitrogen, Mineral and Metal, therefore bridging the gap between diverse disciplines of science and establishing a new relationship between them. His study in the field of Achondrite also crosses realms of Chemical composition. In his work, Kamacite, Diogenite, Howardite and Inclusion is strongly intertwined with Carbonaceous chondrite, which is a subfield of Mineralogy.
The scientist’s investigation covers issues in Chondrite, Geochemistry, Chondrule, Olivine and Meteorite. His Chondrite study integrates concerns from other disciplines, such as Mineralogy, Isotopes of oxygen and Silicate. His work in Geochemistry addresses issues such as Ordinary chondrite, which are connected to fields such as Asteroid.
His study in Chondrule is interdisciplinary in nature, drawing from both Carbonaceous chondrite, Formation and evolution of the Solar System, Cryptocrystalline and Analytical chemistry. His work in Olivine tackles topics such as Forsterite which are related to areas like Melilite. His study on Achondrite and Acapulcoite is often connected to Chemical composition, Martian and Archaeology as part of broader study in Meteorite.
Chondrite, Chondrule, Geochemistry, Olivine and Isotopes of oxygen are his primary areas of study. His study with Chondrite involves better knowledge in Astrobiology. His research integrates issues of Plagioclase and Silicate in his study of Chondrule.
His work on Breccia as part of his general Geochemistry study is frequently connected to Metal, thereby bridging the divide between different branches of science. His Olivine research incorporates elements of Carbonaceous chondrite and Parent body. His research in Isotopes of oxygen intersects with topics in Radiochemistry and Analytical chemistry.
Michael K. Weisberg mainly investigates Chondrule, Chondrite, Plagioclase, Geochemistry and Olivine. His Chondrule research is within the category of Meteorite. In general Meteorite study, his work on Acapulcoite and Achondrite often relates to the realm of Chemical groups, thereby connecting several areas of interest.
He combines subjects such as Comet, Pyroxene, Formation and evolution of the Solar System and Silicate with his study of Analytical chemistry. His work in Mineralogy is not limited to one particular discipline; it also encompasses Porosity. While working on this project, Michael K. Weisberg studies both Isotopes of oxygen and Secondary ion mass spectrometry.
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The CR (Renazzo-type) carbonaceous chondrite group and its implications
Michael K Weisberg;Martin Prinz;Robert N Clayton;Toshiko K Mayeda.
Geochimica et Cosmochimica Acta (1993)
The CR chondrite clan: Implications for early solar system processes
Alexander N. Krot;Anders Meibom;Michael K. Weisberg;Michael K. Weisberg;Klaus Keil.
Meteoritics & Planetary Science (2002)
Mineralogy of carbonaceous chondrite clasts in HED achondrites and the Moon
Michael E. Zolensky;Michael K. Weisberg;Paul C. Buchanan;David W. Mittlefehldt.
Meteoritics & Planetary Science (1996)
Petrology of ALH85085: a chondrite with unique characteristics
Michael K. Weisberg;Michael K. Weisberg;Martin Prinz;Cherukupalli E. Nehru;Cherukupalli E. Nehru.
Earth and Planetary Science Letters (1988)
A new metal-rich chondrite grouplet
Michael K. Weisberg;Michael K. Weisberg;Martin Prinz;Robert N. Clayton;Toshiko K. Mayeda.
Meteoritics & Planetary Science (2001)
Amoeboid olivine aggregates and related objects in carbonaceous chondrites: records of nebular and asteroid processes
Alexander N. Krot;Michail I. Petaev;Sara S. Russell;Shoichi Itoh;Shoichi Itoh.
Chemie Der Erde-geochemistry (2004)
Origin of ureilites inferred from a SIMS oxygen isotopic and trace element study of clasts in the Dar al Gani 319 polymict ureilite
Noriko T. Kita;Yukio Ikeda;Shigeko Togashi;Yongzhong Liu.
Geochimica et Cosmochimica Acta (2004)
Fe‐Ni metal in primitive chondrites: Indicators of classification and metamorphic conditions for ordinary and CO chondrites
M. Kimura;J. N. Grossman;M. K. Weisberg;M. K. Weisberg.
Meteoritics & Planetary Science (2008)
The Carlisle Lakes-type chondrites: A new grouplet with high Δ17O and evidence for nebular oxidation
Michael K. Weisberg;Michael K. Weisberg;Martin Prinz;Hideyasu Kojima;Keizo Yanai.
Geochimica et Cosmochimica Acta (1991)
Oxygen isotope ratios of FeO-poor chondrules in CR3 chondrites: Influence of dust enrichment and H2O during chondrule formation
Travis J. Tenner;Daisuke Nakashima;Takayuki Ushikubo;Noriko T. Kita.
Geochimica et Cosmochimica Acta (2015)
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