Geochemistry, Mineralogy, Quartz, Metamorphic rock and Phengite are his primary areas of study. Geochemistry is often connected to Coesite in his work. His biological study spans a wide range of topics, including Micro raman and Diamond.
The various areas that Hans-Joachim Massonne examines in his Quartz study include Mineral and Continental crust. Hans-Joachim Massonne has researched Metamorphic rock in several fields, including Eclogite and Mantle wedge. Hans-Joachim Massonne interconnects Assemblage and Phlogopite in the investigation of issues within Phengite.
Hans-Joachim Massonne mainly focuses on Geochemistry, Metamorphic rock, Metamorphism, Phengite and Eclogite. His Geochemistry study frequently involves adjacent topics like Terrane. The Metamorphic rock study combines topics in areas such as Massif, Felsic, Biotite and Mineralogy.
Hans-Joachim Massonne combines subjects such as Mylonite, Shear zone and Granulite with his study of Metamorphism. His study in Phengite is interdisciplinary in nature, drawing from both Quartz, Paragonite and Phlogopite. His work deals with themes such as Amphibole and Partial melting, which intersect with Eclogite.
Hans-Joachim Massonne focuses on Geochemistry, Metamorphic rock, Metamorphism, Eclogite and Monazite. His Geochemistry research includes themes of Phengite and Terrane. His Metamorphic rock study integrates concerns from other disciplines, such as Nappe, Epidote, Craton and Massif.
The study incorporates disciplines such as Mylonite, Shear zone, Granulite and Felsic in addition to Metamorphism. His Eclogite research is multidisciplinary, relying on both Petrology and Amphibole. His work focuses on many connections between Paragonite and other disciplines, such as Zoisite, that overlap with his field of interest in Mineralogy.
The scientist’s investigation covers issues in Geochemistry, Metamorphic rock, Monazite, Metamorphism and Zircon. In his works, he performs multidisciplinary study on Geochemistry and High pressure. His biological study spans a wide range of topics, including Schist, Paleozoic, Cretaceous, Precambrian and Gneiss.
In Gneiss, Hans-Joachim Massonne works on issues like Sillimanite, which are connected to Geochronology and Crust. His study in the fields of Fission track dating under the domain of Zircon overlaps with other disciplines such as Proxy. As a part of the same scientific family, he mostly works in the field of Staurolite, focusing on Terrane and, on occasion, Phengite.
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Phengite geobarometry based on the limiting assemblage with K-feldspar, phlogopite, and quartz
Hans Joachim Massonne;Werner Schreyer.
Contributions to Mineralogy and Petrology (1987)
Thermodynamic properties of white micas on the basis of high-pressure experiments in the systems K2OMgOAl2O3SiO2H2O and K2OFeOAl3O3SiO2H3O
Hans-Joachim Massonne;Zbigniew Szpurka.
Lithos (1997)
Diapirs as the source of the sediment signature in arc lavas
Mark D. Behn;Peter B. Kelemen;Greg Hirth;Bradley R. Hacker.
Nature Geoscience (2011)
Microdiamond daughter crystals precipitated from supercritical COH + silicate fluids included in garnet, Erzgebirge, Germany
Bernhard Stöckhert;Johannes Duyster;Claudia Trepmann;Hans-Joachim Massonne.
Geology (2001)
Stability field of the high-pressure assemblage talc+phengite and two new phengite barometers
Hans-Joachim Massonne;Werner Schreyer.
European Journal of Mineralogy (1989)
A comparison of the evolution of diamondiferous quartz-rich rocks from the Saxonian Erzgebirge and the Kokchetav Massif: are so-called diamondiferous gneisses magmatic rocks?
Hans-Joachim Massonne.
Earth and Planetary Science Letters (2003)
Microdiamonds from the Saxonian Erzgebirge, Germany: in situ micro-Raman characterisation
Lutz Nasdala;Hans-Joachim Massonne.
European Journal of Mineralogy (2000)
History of crustal growth and recycling at the Pacific convergent margin of South America at latitudes 29°–36° S revealed by a U–Pb and Lu–Hf isotope study of detrital zircon from late Paleozoic accretionary systems
A.P. Willner;A.P. Willner;A. Gerdes;H.-J. Massonne.
Chemical Geology (2008)
A counterclockwise PTt path of high-pressure/low-temperature rocks from the Coastal Cordillera accretionary complex of south-central Chile: constraints for the earliest stage of subduction mass flow
A.P. Willner;J. Glodny;T.V. Gerya;T.V. Gerya;E. Godoy.
Lithos (2004)
Microdiamonds from the Saxonian Erzgebirge, Germany: in situ micro-Raman characterisation;Microdiamonds from the Saxonian Erzgebirge, Germany: in situ micro-Raman characterisation
Lutz Nasdala;Hans-Joachim Massonne.
European Journal of Mineralogy (2000)
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