Lithospheric density model along the CEL09 profile and its geological implications

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F21%3A00550117" target="_blank" >RIV/67985530:_____/21:00550117 - isvavai.cz</a>

Výsledek na webu

<a href="http://www.geologicacarpathica.com/browse-journal/volumes/72-6/article-991/" target="_blank" >http://www.geologicacarpathica.com/browse-journal/volumes/72-6/article-991/</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.31577/GeolCarp.72.6.1" target="_blank" >10.31577/GeolCarp.72.6.1</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Lithospheric density model along the CEL09 profile and its geological implications

Popis výsledku v původním jazyce

We present a new 2D lithospheric density model along the seismic profile CEL09 crossing the Bohemian Massif, the Western Carpathians, and the Pannonian Basin. The resulting model consists of five principal layers: sediments, upper crust, lower crust, lower lithosphere, and asthenosphere. The thicknesses of the Neogene sedimentary basins vary from 0 to similar to 5.5 km while the Paleogene flysch sediments dip to a depth of similar to 6.5 km. The most complex upper part of the upper crust in the Bohemian Massif is represented mainly by low-density granitoid plutons (similar to 2.60-2.68 g cm(-3)), metamorphic rocks (similar to 2.69-2.74 g cm(-3)) and high-density basic and ultrabasic bodies (similar to 2.78-2.79 g cm(-3)). In the Western Carpathians, this layer is formed by the crystalline Male Karpaty Mts. (2.66-2.67 g cm(-3)), Trans-Danubian range (2.73-2.74 g cm(-3)), and the pre-Cainozoic basement of the sedimentary basins (2.67-2.74 g cm(-3)). The densities of the lower part of the upper crust range from 2.78 g cm(-3) (in the Western Carpathian-Pannonian region) to 2.77-2.80 g cm(-3) (in the Bohemian Massif). In the lower crust, four different sectors were modelled. In the Saxothuringian, they are divided into two layers, the upper layer (2.84-2.85 g cm(-3)) and the lower layer (3.12 g cm(-3)). The Moldanubian has the thickest lower crust (similar to 20 km) with a density of 2.98 g cm(-3). The lower crust in the Moravo-Silesian has a density of 2.97 g cm(-3). The Western Carpathian- Pannonian region is represented by slightly lower densities of 2.94-2.96 g cm(-3). The gravity modelling indicates that the Western Carpathians were overthrusted by similar to 30 km onto the Bohemian Massif resulting in a neo-transformation of the crust/mantle and related lithosphere after subduction.

Název v anglickém jazyce

Lithospheric density model along the CEL09 profile and its geological implications

Popis výsledku anglicky

We present a new 2D lithospheric density model along the seismic profile CEL09 crossing the Bohemian Massif, the Western Carpathians, and the Pannonian Basin. The resulting model consists of five principal layers: sediments, upper crust, lower crust, lower lithosphere, and asthenosphere. The thicknesses of the Neogene sedimentary basins vary from 0 to similar to 5.5 km while the Paleogene flysch sediments dip to a depth of similar to 6.5 km. The most complex upper part of the upper crust in the Bohemian Massif is represented mainly by low-density granitoid plutons (similar to 2.60-2.68 g cm(-3)), metamorphic rocks (similar to 2.69-2.74 g cm(-3)) and high-density basic and ultrabasic bodies (similar to 2.78-2.79 g cm(-3)). In the Western Carpathians, this layer is formed by the crystalline Male Karpaty Mts. (2.66-2.67 g cm(-3)), Trans-Danubian range (2.73-2.74 g cm(-3)), and the pre-Cainozoic basement of the sedimentary basins (2.67-2.74 g cm(-3)). The densities of the lower part of the upper crust range from 2.78 g cm(-3) (in the Western Carpathian-Pannonian region) to 2.77-2.80 g cm(-3) (in the Bohemian Massif). In the lower crust, four different sectors were modelled. In the Saxothuringian, they are divided into two layers, the upper layer (2.84-2.85 g cm(-3)) and the lower layer (3.12 g cm(-3)). The Moldanubian has the thickest lower crust (similar to 20 km) with a density of 2.98 g cm(-3). The lower crust in the Moravo-Silesian has a density of 2.97 g cm(-3). The Western Carpathian- Pannonian region is represented by slightly lower densities of 2.94-2.96 g cm(-3). The gravity modelling indicates that the Western Carpathians were overthrusted by similar to 30 km onto the Bohemian Massif resulting in a neo-transformation of the crust/mantle and related lithosphere after subduction.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10507 - Volcanology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2021

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Geologica Carpathica

ISSN

1335-0552

e-ISSN

1336-8052

Svazek periodika

72

Číslo periodika v rámci svazku

6

Stát vydavatele periodika

SK - Slovenská republika

Počet stran výsledku

14

Strana od-do

447-460

Kód UT WoS článku

000736741100001

EID výsledku v databázi Scopus

2-s2.0-85123780986