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| Content Provider | Springer Nature Link |
|---|---|
| Author | Velledits, Felicitász Blau, Joachim |
| Copyright Year | 2003 |
| Abstract | The present paper presents results of stratigraphical, sedimentological and micropalaeontological investigations of an olistolith from the Büdöskút area in the Bükk Mts (NW Hungary). The olistolith consists of Norian sub- and peritidal platform carbonates (Büdöskút lime-stone). During early diagenesis dissolution cavities originated which where filled by ostracodal mudstones. Other cavities first were wallpapered by evinospongial crusts and later filled either by ostracodal mudstones or by brick-red haematitic material (weathered bauxite). The evinospongial crusts show stromatolite-like structures and their forming therefore is supposed to be organically (microbially) induced.During the Early up to the Late Jurassic the host rock was dissected by neptunian dykes. The internal sediment's faunal content reveals that the dykes formed during the (?) Hettangian/Sinemurian and the Toarcian— Oxfordian age.A comparison of the Büdöskút limestone neptunian dyke internal sediments with the Bükk parautochthonous and the Szarvasko-Mónosbél nappe complex sedimentary columns shows no similarities. Therefore the Büdöskút olistolith is interpreted as an exotic body within the Bükk Mts. |
| Starting Page | 23 |
| Ending Page | 48 |
| Page Count | 26 |
| File Format | |
| ISSN | 01729179 |
| Journal | Facies |
| Volume Number | 48 |
| Issue Number | 1 |
| e-ISSN | 16124820 |
| Language | English |
| Publisher | Springer-Verlag |
| Publisher Date | 2003-01-01 |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Olistolith Evinospongial Crusts Neptunian Dykes Internal Sediments Foraminifera Crustacean Microcoprolites Bükk Mts Triassic-Jurassic Biogeosciences Geochemistry Paleontology Sedimentology Ecology |
| Content Type | Text |
| Resource Type | Article |
| Subject | Geology Stratigraphy Paleontology |
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