Subsidence and thermal history of the Tlumacov-1 borehole

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F15%3A00082751" target="_blank" >RIV/00216224:14310/15:00082751 - isvavai.cz</a>

Výsledek na webu

<a href="http://petrol.natur.cuni.cz/ceteg/sites/default/files/images/pdf/abstract-volume-CETEG2015_online.pdf" target="_blank" >http://petrol.natur.cuni.cz/ceteg/sites/default/files/images/pdf/abstract-volume-CETEG2015_online.pdf</a>

DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Subsidence and thermal history of the Tlumacov-1 borehole

Popis výsledku v původním jazyce

This study investigated the burial history of borehole Tlumacov-1 (Tlu-1). Studied borehole is located in the prospection area Vizovice Hills in the East part of Czech Republic. Borehole Tlumacov-1 hit crystalline basement, autochthonous Carpathian foredeep. Alochthonous formations are represented by thrusted unit of pouzdrany unit, submenilitic formation and Zdanice-Hustopece formation. Total drilled depth reached 2315 m. For burial history reconstruction, heat flow (HF) scenario respecting typical HFvalues has been expected basen on Allen ? Allen (2006). Heat flow values stars with XX for Devonian rift. Heat flow increase was followed by continuous cooling up to neogene, when cooling was increased due to Carpathin nappes thrusting. Recent calculatedHF values are XX. Presented study represent forwad burial history reconstruction with several newly measured calibration parameters expressed as the random vitrinite reflectance (Rr).

Název v anglickém jazyce

Subsidence and thermal history of the Tlumacov-1 borehole

Popis výsledku anglicky

This study investigated the burial history of borehole Tlumacov-1 (Tlu-1). Studied borehole is located in the prospection area Vizovice Hills in the East part of Czech Republic. Borehole Tlumacov-1 hit crystalline basement, autochthonous Carpathian foredeep. Alochthonous formations are represented by thrusted unit of pouzdrany unit, submenilitic formation and Zdanice-Hustopece formation. Total drilled depth reached 2315 m. For burial history reconstruction, heat flow (HF) scenario respecting typical HFvalues has been expected basen on Allen ? Allen (2006). Heat flow values stars with XX for Devonian rift. Heat flow increase was followed by continuous cooling up to neogene, when cooling was increased due to Carpathin nappes thrusting. Recent calculatedHF values are XX. Presented study represent forwad burial history reconstruction with several newly measured calibration parameters expressed as the random vitrinite reflectance (Rr).

Druh

O - Ostatní výsledky

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2015

Kód důvěrnosti údajů

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