Schematic geological map (modified after Pícha et al., 2006) with location of the boreholes studied. For borehole numbering see Appendices 1 and 2.

Contexts in source publication

Context 1

... Mio cene de pos its stud ied be long to the Moravian part of the West ern Carpathian Foredeep -a pe riph eral fore land basin formed through the tec tonic em place ment and crustal loading of the West ern Carpathian Thrust Front onto the pas sive mar gin of the Bo he mian Mas sif (Nehyba and Šikula, 2007; Fig. 1). The West ern Carpathian Foredeep con tin ues into the Pol ish Carpathian Foredeep Ba sin north-eastwards (Oszczy pko et al., 2006) and to the North Al pine-Fore land Ba sin (Aus trian Molasse Ba sin/Al pine Molasse Zone) to the south-west. To the east/south-east, the foredeep suc ces sion is over rid den by the West ern Carpathian ...

Context 2

... rocks of Brunovistulicum, De vo nian to Lower Car bon if er ous car bon ates, and Car bon if er ous siliciclastic de pos its -"Culm fa cies" of the Moravian-Silesian Pa leo zoic (Jirman et al., 2018). Ero sional rel ics of Ju ras sic and autochthonous Paleogene strata are also pres ent, es pe cially in the south ern seg ment of the area analysed (Fig. 1) where the Mio cene depositional sys tem over lies the Nesvaèilka and Vranovice palaeovalleys ( Kalvoda et al., 2003Kalvoda et al., , 2008Zágoršek et al., 2012;Hladilová et al., 2014). The base ment gen er ally dips south-eastwards; how ever, the re lief is very ir reg u lar. In the S and SE part of the ba sin the base ment is mostly ...

Context 3

... south ern and north ern seg ments. In to tal, 25 core sam ples from 13 bore holes were se lected for maceral anal y ses and huminite reflectance. An a lyt i cal data ob tained in the past, but never published, are also used in this work. These are the re sults of 135 anal y ses of TOC, 141 Rock-Eval py rol y sis anal y ses from 39 bore holes ( Fig. 1 and Ap pen dix 1), and 27 vitrinite reflectance anal y ses from 18 bore holes ( Fig. 1 and Ap pen dix 2). The huminite/vitrinite reflectance and maceral eval u a tion was car ried out by Olym pus BX51 mi cro scope with a Zeiss Photomultiplier MK3 sys tem, an im mer sion lens with 40x magni fi ca tion, and Pelcon point coun ter. OLYMPUS ...

Context 4

... se lected for maceral anal y ses and huminite reflectance. An a lyt i cal data ob tained in the past, but never published, are also used in this work. These are the re sults of 135 anal y ses of TOC, 141 Rock-Eval py rol y sis anal y ses from 39 bore holes ( Fig. 1 and Ap pen dix 1), and 27 vitrinite reflectance anal y ses from 18 bore holes ( Fig. 1 and Ap pen dix 2). The huminite/vitrinite reflectance and maceral eval u a tion was car ried out by Olym pus BX51 mi cro scope with a Zeiss Photomultiplier MK3 sys tem, an im mer sion lens with 40x magni fi ca tion, and Pelcon point coun ter. OLYMPUS Im mer sion Oil Type-F was used. Ran dom reflectance was de ter mined on polished sec ...

Context 5

... reflectance ranges from 0.34 to 0.58% R r in the north ern seg ment (Fig. 4 and Ap pen dix 2). In bore hole NP-779 (ID 16 in Fig. 1), sit u ated ahead of the West Carpathian orogenic front, ma tu rity reaches 0.36% R r at a depth of 179 m. How ever, the strata in ter sected be neath the Carpathian nappes at a depth of 887 m in bore hole Lhotka-5 (ID 13 in Fig. 1) show a com pa ra ble re flec tivity (0.34% R r ). This sim i lar ity sug gests that the ob served ma tu ...

Context 6

... ranges from 0.34 to 0.58% R r in the north ern seg ment (Fig. 4 and Ap pen dix 2). In bore hole NP-779 (ID 16 in Fig. 1), sit u ated ahead of the West Carpathian orogenic front, ma tu rity reaches 0.36% R r at a depth of 179 m. How ever, the strata in ter sected be neath the Carpathian nappes at a depth of 887 m in bore hole Lhotka-5 (ID 13 in Fig. 1) show a com pa ra ble re flec tivity (0.34% R r ). This sim i lar ity sug gests that the ob served ma tu rity level was reached be fore the Carpathian nappes over rode the Mio cene suc ces sion of the ...

Context 7

... Mio cene de pos its stud ied be long to the Moravian part of the West ern Carpathian Foredeep -a pe riph eral fore land basin formed through the tec tonic em place ment and crustal loading of the West ern Carpathian Thrust Front onto the pas sive mar gin of the Bo he mian Mas sif (Nehyba and Šikula, 2007; Fig. 1). The West ern Carpathian Foredeep con tin ues into the Pol ish Carpathian Foredeep Ba sin north-eastwards (Oszczy pko et al., 2006) and to the North Al pine-Fore land Ba sin (Aus trian Molasse Ba sin/Al pine Molasse Zone) to the south-west. To the east/south-east, the foredeep suc ces sion is over rid den by the West ern Carpathian ...

Context 8

... rocks of Brunovistulicum, De vo nian to Lower Car bon if er ous car bon ates, and Car bon if er ous siliciclastic de pos its -"Culm fa cies" of the Moravian-Silesian Pa leo zoic (Jirman et al., 2018). Ero sional rel ics of Ju ras sic and autochthonous Paleogene strata are also pres ent, es pe cially in the south ern seg ment of the area analysed (Fig. 1) where the Mio cene depositional sys tem over lies the Nesvaèilka and Vranovice palaeovalleys ( Kalvoda et al., 2003Kalvoda et al., , 2008Zágoršek et al., 2012;Hladilová et al., 2014). The base ment gen er ally dips south-eastwards; how ever, the re lief is very ir reg u lar. In the S and SE part of the ba sin the base ment is mostly ...

Context 9

... south ern and north ern seg ments. In to tal, 25 core sam ples from 13 bore holes were se lected for maceral anal y ses and huminite reflectance. An a lyt i cal data ob tained in the past, but never published, are also used in this work. These are the re sults of 135 anal y ses of TOC, 141 Rock-Eval py rol y sis anal y ses from 39 bore holes ( Fig. 1 and Ap pen dix 1), and 27 vitrinite reflectance anal y ses from 18 bore holes ( Fig. 1 and Ap pen dix 2). The huminite/vitrinite reflectance and maceral eval u a tion was car ried out by Olym pus BX51 mi cro scope with a Zeiss Photomultiplier MK3 sys tem, an im mer sion lens with 40x magni fi ca tion, and Pelcon point coun ter. OLYMPUS ...

Context 10

... se lected for maceral anal y ses and huminite reflectance. An a lyt i cal data ob tained in the past, but never published, are also used in this work. These are the re sults of 135 anal y ses of TOC, 141 Rock-Eval py rol y sis anal y ses from 39 bore holes ( Fig. 1 and Ap pen dix 1), and 27 vitrinite reflectance anal y ses from 18 bore holes ( Fig. 1 and Ap pen dix 2). The huminite/vitrinite reflectance and maceral eval u a tion was car ried out by Olym pus BX51 mi cro scope with a Zeiss Photomultiplier MK3 sys tem, an im mer sion lens with 40x magni fi ca tion, and Pelcon point coun ter. OLYMPUS Im mer sion Oil Type-F was used. Ran dom reflectance was de ter mined on polished sec ...

Context 11

... reflectance ranges from 0.34 to 0.58% R r in the north ern seg ment (Fig. 4 and Ap pen dix 2). In bore hole NP-779 (ID 16 in Fig. 1), sit u ated ahead of the West Carpathian orogenic front, ma tu rity reaches 0.36% R r at a depth of 179 m. How ever, the strata in ter sected be neath the Carpathian nappes at a depth of 887 m in bore hole Lhotka-5 (ID 13 in Fig. 1) show a com pa ra ble re flec tivity (0.34% R r ). This sim i lar ity sug gests that the ob served ma tu ...

Context 12

... ranges from 0.34 to 0.58% R r in the north ern seg ment (Fig. 4 and Ap pen dix 2). In bore hole NP-779 (ID 16 in Fig. 1), sit u ated ahead of the West Carpathian orogenic front, ma tu rity reaches 0.36% R r at a depth of 179 m. How ever, the strata in ter sected be neath the Carpathian nappes at a depth of 887 m in bore hole Lhotka-5 (ID 13 in Fig. 1) show a com pa ra ble re flec tivity (0.34% R r ). This sim i lar ity sug gests that the ob served ma tu rity level was reached be fore the Carpathian nappes over rode the Mio cene suc ces sion of the ...