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02541nab a2200289 4500 |
| 003 - CONTROL NUMBER IDENTIFIER |
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GSMBLIc |
| 008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION |
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210224b ||||| |||| 00| 0 eng d |
| 041 ## - LANGUAGE CODE |
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| Language code of text/sound track or separate title |
Einglish Language |
| 100 ## - MAIN ENTRY--PERSONAL NAME |
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| Personal name |
Haas, Janos |
| 9 (RLIN) |
7741 |
| 245 ## - TITLE STATEMENT |
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| Title |
Stratigraphy, facies and geodynamic settings of Jurassic formations in the Bukk mountains, North Hungary : Its relations with the other areas of the Neotethyan realm |
| 300 ## - PHYSICAL DESCRIPTION |
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| Extent |
18-49pp. |
| Other physical details |
Colour illustration |
| 300 ## - PHYSICAL DESCRIPTION |
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| Other physical details |
maps |
| 520 ## - SUMMARY, ETC. |
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| Summary, etc. |
Jurassic mélange complexes related to the subduction of the Neotethys Ocean occur in the Bükk Mountains, North Hungary. This paper characterizes the sedimentary sequence of basin and slope facies that occur in the southwestern part of the Bükk Mountains, placing special emphasis on the redeposited sedimentary rocks (olistostromes, olistoliths: Mónosbél Group) in order to obtain information on the provenance of the clasts, and the mode and time of their redeposition. The series of formations studied shows a general coarsening-upwards trend. Based on radiolarians and foraminifera, the Mónosbél Group formed in Early to Late Bathonian time. The lower part of the complex is typified by a predominance of pelagic carbonates, shale and radiolarite with andesitic volcaniclastic intercalations. The higher part of the succession is characterized by polymictic olistostromes. Large olistoliths that are predominantly blocks of Bathonian shallow marine limestone (Bükkzsérc Limestone) appear in the upper part of the sequence. Based on the biostratigraphic and sedimentological data, results of analyses of the redeposited clasts and taking into consideration the concepts of the development of the western Neotethys domain, the evolutionary stages of the sedimentary basins were defined. The onset of the compressional stage led to initiation of nappe stacking that led to the formation of polymict olistostromes and then to the redeposition of large blocks derived from out-of-sequence nappes of the former platform foreland. |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
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| Topical term or geographic name entry element |
Gravity deposits |
| 9 (RLIN) |
7742 |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
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| Topical term or geographic name entry element |
Polymictic olistostrome |
| 9 (RLIN) |
8791 |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
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| Topical term or geographic name entry element |
Subduction |
| 9 (RLIN) |
8629 |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
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| Topical term or geographic name entry element |
Neotethys |
| 9 (RLIN) |
8792 |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
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| Topical term or geographic name entry element |
Biostraigraphy |
| 9 (RLIN) |
7779 |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
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| Topical term or geographic name entry element |
Foraminifera |
| 9 (RLIN) |
8793 |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
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| Topical term or geographic name entry element |
Radiolaria |
| 9 (RLIN) |
2660 |
| 700 ## - ADDED ENTRY--PERSONAL NAME |
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| Personal name |
Pelikan, Pal |
| 9 (RLIN) |
7746 |
| 700 ## - ADDED ENTRY--PERSONAL NAME |
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| Personal name |
Gorog, Agnes |
| 9 (RLIN) |
7747 |
| 700 ## - ADDED ENTRY--PERSONAL NAME |
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| Personal name |
Jozsa, Sandor |
| 9 (RLIN) |
7748 |
| 700 ## - ADDED ENTRY--PERSONAL NAME |
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| Personal name |
Ozsvart, Peter |
| 9 (RLIN) |
1490 |
| 773 0# - HOST ITEM ENTRY |
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| Host Biblionumber |
1897 |
| Host Itemnumber |
2185 |
| Place, publisher, and date of publication |
London Cambridge University Press 2013 |
| Other item identifier |
002531 |
| Title |
Geological magazine : Vol. 150 Iss. 1-6 Year. 2013 |
| International Standard Serial Number |
00167568 |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) |
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| Source of classification or shelving scheme |
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| Call number suffix |
{082b} |
| Koha item type |
Article |
