Wybrane parametry fizyczne minerałów i skał w funkcji ciśnienia i temperatury oraz ich przydatność do interpretacji danych geofizycznych

Bakun-Czubarow, N.

Artykuł - szczegóły

Tytuł artykułu

Wybrane parametry fizyczne minerałów i skał w funkcji ciśnienia i temperatury oraz ich przydatność do interpretacji danych geofizycznych

Autorzy

Bakun-Czubarow N.

Wybrane pełne teksty z tego czasopisma

http://www.pgi.gov.pl/oferta-inst/wydawnictwa/serie-wydawnicze/prace-pig.html

Identyfikatory

Warianty tytułu

Selected physical parameters of minerals and rocks versus pressure and temperature, their usefulness in interpretation of geophysical data

Języki publikacji

Abstrakty

Petrologiczno-geologiczna interpretacja profili sejsmicznych litosfery jest możliwa dzięki stosowaniu wyników pomiarów laboratoryjnych parametrów fizycznych minerałów i skał. Podstawowymi parametrami fizycznymi czułymi na zmiany składu chemicznego są prędkości propagacji fal sejsmicznych (Vp i Vs) oraz gęstość (r). W badaniach litosfery powinien być także uwzględniany parametr k = Vp/Vs i anizotropia sejsmiczna. Celem pracy było zgromadzenie wybranych parametrów fizycznych głównych minerałów i skał litosfery z całego świata oraz próba prześledzenia zmienności tych parametrów w funkcji ciśnienia i temperatury. Parametry fizyczne zestawiono w pięciu tabelach, z których cztery poświęcono skałom, a jedną anizotropii Vp w monokryształach minerałów. Modele petrologiczne litosfery powinny charakteryzować się zgodnością wydzieleń litologicznych z profilami sejsmicznymi, a także wykazywać zgodność z geologią, tektoniką i dostępnym inwentarzem skalnym obszaru modelowania. W petrologicznym modelowaniu litosfery powinna być uwzględniana natura nieciągłości geofizycznych (nieciągłości składu chemicznego, transformacje fazowe bądź zmiany stanu skupienia). Natura nieciągłości Moho pozostaje ciągle przedmiotem dyskusji i na znacznych obszarach ma, najprawdopodobniej, charakter transformacji typu gabro→eklogit.

Application of the results of small scale laboratory determinations of physical parameters of minerals and rocks made possible to perform a petrological and geological interpretation of seismic profiles of lithosphere. Seismic velocities (V_p and V_s) as well as density (p) are the main physical parameters that are sensitive to changes of chemical composition of minerals and rocks. In lithospheric studies the k = V_p/V_s parameter should be also considered as well as seismic anisotropy. The aim of the paper was to compile selected physical parameters of major minerals and lithospheric rocks from all over the world, as well as to present their changes as function of pressure and temperature. Physical parameters are collected in five tables, four of which are devoted to rocks and the fifth one - to the Vp anisotropy of single crystals of major minerals. For these minerals, there are also given mean values of densities as well as P- and S-wave velocities. In petrological modelling of Earth's crust and mantle, the concordance with tectonics, geology and rocks available in the area, as well as the nature of seismic discontinuities should be considered. The idea that Moho discontinuity has the nature of gabbro → eclogite transformation is postulated. Moreover, the position of phase separation boundaries strongly depends upon chemical composition of the rocks.

Słowa kluczowe

fale sejsmiczne P i S prędkość propagacji gęstość minerałów gęstość skał parametr Vp/Vs anizotropia modelowanie petrologiczne górny płaszcz skorupa

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Prace Państwowego Instytutu Geologicznego

Rocznik

2006

Tom

T. 188

Strony

9--24

Opis fizyczny

Biblogr. 72 poz.

Twórcy

autor

Bakun-Czubarow N.

nbakun@twarda.pan.pl

Instytut Nauk Geologicznych Polskiej Akademii Nauk, ul. Twarda 51/55, 00-818 Warszawa

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