Mihai Ducea

The Nordfjord-Sogn Detachment Zone of western Norway represents an archetype for crustal-scale normal faults that are typically cited as one of the primary mechanisms responsible for the exhumation of ultrahighpressure (UHP) terranes. In this paper, we investigate the role of normal-sense shear zones with respect to UHP exhumation using structural geology, thermobarometry, and geochronology of the Hornelen segment of the Nordfjord-Sogn Detachment

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Poziția Asociației „Ad Astra” a Cercetătorilor din România privind încălcările tot mai frecvente ale eticii academice în publicațiile științifice

Observatii privind proiectul legii cercetatorului, aflat in discutie publica

Probleme ale legii statutului cercetătorului şi ale legii eticii cercetării

Articolele autorului Mihai Ducea
Link la profilul stiintific al lui Mihai Ducea

Cyclicity in Cordilleran Orogenic systems

Characterization of the crust of the Coast Mountains Batholith, British Columbia, from P to S converted seismic waves and petrologic modeling

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U-Pb geochronology of granitoids in the north-western boundary of the Xolapa terrane

Kinematic history of the Fuegian Andes as indicated by U-Pb detrital-zircon geochronology and rare earth element geochemistry of the Magallanes foreland basin

Chronology of pluton emplacement and regional deformation in the southern Sierra Nevada Batholith, California

Temporal-compositional trends over short and long time-scales in basalts of the Big Pine volcanic field, California

Preliminary stratigraphic and structural architecture of Bhutan: Implications for the along strike architecture of the Himalayan system

Exhumation of ultrahigh-pressure rocks beneath the Hornelen segment of Norvegian Caledonides

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