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
See also Barbados Accretionary Prism (BAP) Calabrian 225-226, 254 evaporite deposits in 254 formation of 224 Makran 399 Mediterranean 253, 265 in Northern South America 145 active diapirism 304, 368, 442 active fold-thrust belt in Zagros region 35-36 active salt diapirism 337, 439 Adriatic Sea 216-217, 221, 251, 253, 264 arc-ridge systems in 219 Southern 230, 244, 254 Aegean Sea 220-221, 224, 254, 257 Hellenic trench south of 216 northern and eastern shores of 219 to south Anatolia region 220 subduction zone south of 258 Afar plume 9, 14, 16 Afar region 34 active volcanoes in 415 Afar Volcanic Province 15, 17 in Africa 5, 10 Danakil Depression in 7, 393 in Ethiopia 11, 15 magmatic activity in 25 in northern Africa 14, 95 volcanic activity in 23 volcanic complexes in 416 in Yemeni highlands 15 African-Anatolian plate boundary 258 African cratonic blocks 94 African margin north of Angola 101 African Plate 3, 28, 35, 94, 111, 144, 215, 224, 474 in Gulf of Aden region 10 NW 156 subduction of 220, 254 submarine prolongation of 219 Alaminos Canyon region 196 Alberta Basin, Canada, salt dissolution in 419-424 Albian carbonate platform 100, 120, 346 Albian carbonate rocks 90, 108, 115, 117 fault zones translated blocks of 109 turtleback structure formed by 306 Albian gap 114, 122, 123, 124, 124-125 Albian marine carbonate sediments 5 Alboran Sea 216, 218, 245, 395 to Corsica and Sardinia islands 244 Strait of Gibraltar at 219 Western 220 Algerian Basin 220, 244-246 Algero-Balearic basin 219, 251 Alice Springs Orogeny 471 allochthonous salt bodies 127, 320, 350 distinct tiers of 179 in Gulf of Mexico 189 in Neogene layers 224 proximal 178 in Sigsbee Escarpment region 192 allochthonous salt masses 16, 20, 23, 27, 179, 195, 334, 416, 504 megabreccias 469 on pre-salt basement 148 salt tectonics in 294 sourced from Hormuz salt diapirs 371 by thrust fault 288 allochthonous salt structures 175, 178, 183, 186, 188, 192, 333, 337-338, 344, 381, 418, 440 development of 339 features associated with 341 in Gulf of Mexico 370-372 in sedimentary basins 339, 368-373 structures associated with 340 submarine 307 allochthonous salt tongues 118-119, 132, 154, 170, 179, 182, 185, 288, 302, 307, 312, 377 characterization of compressional structures and 176 escarpment results from 147 fold-thrust belt in 152 formation of 294 in Gulf of Mexico 371 models 279 in Sigsbee Escarpment and abyssal plain 172 Alpine fold-thrust belts 216 Alps 219, 224, 281, 288 to Anatolia 222 in central Europe 278 Danakil 7 Western 336 to Zagros region 216 Amadeus evaporite basin 469, 471 Ambal Ridge 363-364, 419, 420 Amber-1 exploratory well 16, 29 American Association of Petroleum Geologists (AAPG) 155, 278-279 Anatolian block 216, 257 Andean Altiplano 492-493 lithium saltworks 495 Salar de Atacama in 495-497 simplified geological map 496 Andean Ranges in South America 492 Angola basins 93 Angolan margins 105, 132, 294, 345, 346 deep seismic reflection and refraction profiles in 107 salt diapirs on 434 southern segment of 112 antithetic faults 190, 299-300, 311-312, 334, 403.See also extensional faults with allochthonous salt lenses 313 with basal shear zones 122 Apalachicola Embayment 163, 186, 191 Apennine Mountains in Central Italy 218 in Italian Peninsula 235 Apennines 216, 224, 231 evaporite outcrops 264 fold-thrust belt 251 N-S trending 219 stratigraphic successions in Italy 485 subduction zone 246 Appalachian fold-thrust belt 149,
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 | 0.001 |
| Meta-epidemiology (broad) | 0.001 | 0.001 |
| Bibliometrics | 0.001 | 0.003 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.001 | 0.000 |
| Research integrity | 0.001 | 0.002 |
| Insufficient payload (model declined to judge) | 0.004 | 0.474 |
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