High frequency subtidal-peritidal cycles of the Callovian Calabozo Formation (Neuquén Basin, Western Argentina): Preliminary approach
The Calabozo Formation (Cuyo Mesosequence, Neuquén Basin) is made up by a thin, up to 30-m thick Middle Jurassic carbonate-dominated sequence. The minor, thin siliciclastic facies in this formation (i.e. lowermost granule-pebble shoreface conglomerate and fine-grained sandstones interbedded among th...
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2005
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| LEADER | 11819caa a22009017a 4500 | ||
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| 001 | PAPER-4071 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518203335.0 | ||
| 008 | 190411s2005 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-20644459719 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Palma, R.M. | |
| 245 | 1 | 0 | |a High frequency subtidal-peritidal cycles of the Callovian Calabozo Formation (Neuquén Basin, Western Argentina): Preliminary approach |
| 260 | |c 2005 | ||
| 270 | 1 | 0 | |m Palma, R.M.; Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Pabellón II, 1428 Buenos Aires, Argentina; email: palma@gl.fcen.uba.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a The Calabozo Formation (Cuyo Mesosequence, Neuquén Basin) is made up by a thin, up to 30-m thick Middle Jurassic carbonate-dominated sequence. The minor, thin siliciclastic facies in this formation (i.e. lowermost granule-pebble shoreface conglomerate and fine-grained sandstones interbedded among the lower carbonates) record early transgressive shoreline and shallow lagoonal-subtidal sedimentation, respectively. The major carbonate deposits have been split into six facies and seven microfacies on the base of macroscopic field observation and petrological analysis. The carbonate facies have been grouped into three major assemblages: 1) Tidal flat facies assemblage (including the planar laminated algal boundstone facies; 2) Inner platform facies assemblage (including peloidal and bioclastic wackestone, coral floatstone and bioclastic and intraclastic packstone facies; and 3) Platform margin assemblage (including oolitic-peloidal packstone-grainstone facies). A fossil algal record made up by dasycladacean species (Salpingoporella annulata, Cylindroporella sp. and Heteroporella sp.) and blue-green algae (Cayeuxia (Rivularia) piae, and Cayeuxia (Rivularia) kurdistanensis) has been reported for the first time in this unit. The analysis of the intracycle facies and microfacies arrangements, as well as the nature of the cycle bounding surfaces, enabled one to identify two kinds of cycles. 1) Widespread subtidal cycles capped by shallow to intermediate subtidal facies, with no evidence of subaerial exposure at cycle tops; and 2) a minor subtidal cycle with similar shallowing-upward trend but capped by peritidal facies. The stacking pattern and thickness trend of these cycles was studied to determine possible allocyclic and autocyclic controls on their evolution. The Fischer plots reveal that the deposition of the Calabozo Formation subtidal-peritidal cycles took place under upward decreasing accommodation space conditions which may be related to eustatic lowering. © UB-ICTJA. |l eng | |
| 593 | |a Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Pabellón II, 1428 Buenos Aires, Argentina | ||
| 593 | |a UBA-CONICET, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Pabellón II, 1428 Ciudad Autonoma de Buenos Aires, Argentina | ||
| 593 | |a Université Ibn Tofail, Faculté des Sciences, Department of Geologie, BP. 133, Kénitra, Morocco | ||
| 690 | 1 | 0 | |a CARBONATE FACIES AND MICROFACIES |
| 690 | 1 | 0 | |a JURASSIC |
| 690 | 1 | 0 | |a SUBTIDAL-PERITIDAL CYCLICITY |
| 690 | 1 | 0 | |a FACIES ANALYSIS |
| 690 | 1 | 0 | |a WESTERN HEMISPHERE |
| 690 | 1 | 0 | |a WORLD |
| 690 | 1 | 0 | |a ALGAE |
| 690 | 1 | 0 | |a ANTHOZOA |
| 690 | 1 | 0 | |a CHLOROPHYTA |
| 690 | 1 | 0 | |a CYANOBACTERIA |
| 690 | 1 | 0 | |a CYLINDROPORELLA |
| 690 | 1 | 0 | |a UNCULTURED CYANOBACTERIUM |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a NEUQUEN BASIN | |
| 651 | 4 | |a SOUTH AMERICA | |
| 700 | 1 | |a Lo Forte, G.L. | |
| 700 | 1 | |a Medhli, M. | |
| 700 | 1 | |a Piethé, R.D. | |
| 773 | 0 | |d 2005 |g v. 3 |h pp. 119-132 |k n. 2 |p Geol. Acta |x 16956133 |w (AR-BaUEN)CENRE-8135 |t Geologica Acta | |
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