P-wave velocity anisotropy determined on amphibolite samples from a borehole in the Rataje zone of Kutná Hora crystalline complex

0572108 - GFÚ 2024 CZ eng J - Článek v odborném periodiku
Vajdová, Veronika
P-wave velocity anisotropy determined on amphibolite samples from a borehole in the Rataje zone of Kutná Hora crystalline complex.
Acta Universitatis Carolinae. Geologica. Roč. 41, č. 2 (1997), s. 95-100. ISSN 0001-7132
Grant CEP: GA AV ČR IAA3012603
Institucionální podpora: RVO:67985530
Klíčová slova: elastic waves * velocity * Kutná Hora crystalline complex
Obor OECD: Volcanology
Způsob publikování: Omezený přístup

Velocity of elastic waves is an important physical parameter of rocks. This parameter depends on density, mineralogical composition, elastic properties of rockforming minerals, crystallographic preferred orientation, grain shape, grain size, defects of grains, on pore characteristics including volume of pore space, on pore preferred orientation and fluid saturation, and on external factors such as pressure and temperature.
Trvalý link: https://hdl.handle.net/11104/0342935