Miocene to recent stratigraphy, structural arcitecture and tectonic evolution of the florence rise, Eastern Mediterranean sea
Why this work is in the frame
A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.
Bibliographic record
Abstract
Dokuz Eyl?l ?niversitesi ve Newfoundland Memorial ?niversitesi (MUN) taraf?ndan 2007 y?l?n?n yaz?nda, Do?u Akdeniz'deki Floransa Y?kselimi hakk?nda yeni ?ok kanall? sismik veriler elde edilmi?tir. T?rkiye'nin g?neyinde, Do?u Akdeniz'de yer alan Floransa Y?kselimi'nin Miyosen d?neminden bug?ne kadarki yap?sal mimarisi, tektonik ve evrimi, yakla??k 700 km boyunca y?ksek ??z?n?rl?kl?, ?ok kanall? sismik yans?ma profillerinin detayl? ?ekilde yorumlanmas? sonucunda sunulmu?tur. ?? sismik stratigrafik birim tespit edilmi?tir. Birinci birim Pliyosen-Kuvaterner i?erisinde 1a, 1b ve 1c olarak adland?r?lan, ?nemli ?l??de do?rusal devaml?l?k g?steren ?? alt birimden olu?an, g??l? refleksiyon veren akustik bir paket ile karakterize edilmektedir.Yap?sal ve stratigrafik yorumlar, Floransa T?mse?i'nin d?rt yap?sal alana b?l?nebilece?ini ortaya koymaktad?r: a) birinci alan ? kuzeyde, hakim olaran g?neye uzanan bindirmelere sahip tuz ?zl? b?k?lme ku?a??, Antalya havzas?na do?ru uzanmaktad?r; b) ikinci alan ? k?vr?ml? deniz taban? yap?lar? g?steren Pliyosen ?ncesi ? Kuvaterner yap?lar??M? reflekt?r?nde tuz tektoni?inden kaynaklanan ve nedeni henuz a??klamam?? ters d?nm?? yap?lardan olu?maktad?r. Bu alanda dar (1 kilometre geni?li?inde) kesinti zonlar?, y?ksek a??l? faylarla s?n?rlanm?? basen inversiyon yap?lar? olarak yorumlanabilir; c) ???nc? alan ? Floransa Y?kselimi'nin g?neyinde, Pliyosen-Kuvaterner i?erisinde b?y?me yap?lar? (grow strata wedges) olan, 15-20 kilometrelik batimetrik bir y?kselim, karma??k faylanmaya sahip bant zonu ve Floransa T?mse?i'nin merkezinde k?vr?mlanm?? fayl? kayma zonu yer almaktad?r; d) d?rd?nc? alan ? yanal at?ml? ku?ak olarak tan?mlanan bu alan birinci alan ile benzer morfolojik ?zellikler g?stermekte ve yanal at?ml? faylar ile s?n?rl? degi?ken k?vr?ml? deniz taban? yap?s? sunmaktad?r. New multi-channel seismic data were acquired by Dokuz Eyl?l University and Memorial University of Newfoundland (MUN) over the Florence Rise, eastern Mediterranean Sea, during the summer of 2007. The Miocene-Recent structural architecture, tectonic and sedimentary evolution of the Florence Rise south of Turkey in the eastern Mediterranean Sea is delineated using detailed interpretation of ~700 km of high-resolution multi-channel seismic reflection profiles. Three seismic stratigraphic units are identified. Unit 1 is Pliocene-Quaternary in age and is characterized by a strongly reflective acoustic package which shows considerable lateral continuity and three subunit which 1a,1b,1c identified in Unit 1. Unit 2 is generally characterized by a low reflectivity package with weak and often discontinuous reflections: it represents the Messinian evaporite succession and two subunit which 2a, 2b are identified in Unit 2. Unit 3 underlies the Messinian evaporites of Unit 2, and constitutes the acoustic basement in the study area.Analysis of structural and stratigraphic architectures reveals that the Florence Rise can be divided into four structural domains: a) Domain 1- In the north, the salt cored fold belt, with predominantly (but not ubiquitously) south-verging thrusts, extends into the Antalya Basin b) Domain 2- is composed of a broad corrugated seafloor high, in which the corrugations are mirrored at the pre-Pliocene-Quaternary `M? reflector. Narrow (1 km-wide) zones of discontinuity in this area may be interpreted as basin inversion structures bounded by high-angle faults. c) Domain 3- To the south of the broad core of Florence Rise, lies a 15-20 km bathymetric high zone of complexly faulted slivers with Pliocene-Quaternary growth strata wedges and the folded faulted and shear zone in core of the Florence Rise, d) Domain 4- the strike slip belt.
Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.
Full frame distilled prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.001 | 0.000 |
| Meta-epidemiology (broad) | 0.001 | 0.000 |
| Bibliometrics | 0.000 | 0.001 |
| Science and technology studies | 0.001 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.001 |
| Insufficient payload (model declined to judge) | 0.000 | 0.000 |
Machine scores (provisional)
The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.
Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it