- Page 1 and 2: IChlor « Nikoiov THE MEDITERRANEAN
- Page 3 and 4: Todor G. Nikolov LE CRETACE INFERIE
- Page 5 and 6: In this monograph the Lower Cretace
- Page 7: ficiently investigated. On the othe
- Page 11 and 12: eds formed during the Early Cretace
- Page 13 and 14: Table 2 The Early Cretaceous Time S
- Page 15 and 16: already defined stages and led to t
- Page 17 and 18: Table 3 Biostratigraphic Zones in t
- Page 19 and 20: Table 5 Nannoplanklon Zones in the
- Page 21 and 22: Table 6 Concurrent-Range-Zones in V
- Page 23 and 24: S. verrucosum Zone. It is based on
- Page 25 and 26: 2.3.2. Biostratigraphic Zones The b
- Page 27 and 28: The zone is characterized by S. say
- Page 29 and 30: С. emerici has not been found in t
- Page 31 and 32: (U h 1.), M. soulieri (Mat h.), M.
- Page 33 and 34: Table 10 Ammonite Zones in Aptian (
- Page 35 and 36: Table 11 The Foraminifera-Zones in
- Page 37 and 38: English literature with the name "G
- Page 39 and 40: H. dentatus Zone. It is based on th
- Page 41 and 42: Part Two REGIONAL STRATIGRAPHY III.
- Page 43 and 44: Fig. 3. Map of the distribution of
- Page 45 and 46: formation (mails with rare intercal
- Page 47 and 48: limestones, clayey and sandy limest
- Page 49 and 50: gressiveiy and discordantly by pala
- Page 51 and 52: and Salas Formations, and on the ot
- Page 53 and 54: Requienia zlatarskii P a q., Mather
- Page 55 and 56: Albian deposits in this region are
- Page 57 and 58: To the east of Osâm river Hauteriv
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Fig. 9. Section of the LoveC Urgoni
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zonality of tlic Bcrriasian sedimen
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In the Oniurtag and Preslav anticli
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To the southwest and south of Dobri
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tion there are impure calcareous sa
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In the Lorn Depression the Lower Cr
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the Berriasian is represented by a
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a gradual lithological transition,
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Slightly calcareous to slightly ale
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50-60 m thick) of the Kaspican Form
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The thickness of the Barremian depo
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The thickness of the Bedoulian in t
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Together with the ammonites, the Al
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Specificilly good faunistic success
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cf. hitzeli J a c, Costidiscus rect
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stones, reddish marls, sandy-clayey
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of alternation of marls and clayey
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Characteristic Upper Albian ammonit
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three ammonite zones of the Berrias
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qiiadratus Sayn, N. (Tescheniic-s)
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doba, Jaen, Alicante and on the Bal
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Table 15 Major Lithostratigraphic U
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zones: from the Nannocomts colomi Z
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nites decrease, while bivalvs and e
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6. SWISS ALPS In addition to Jura M
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The Strambach Limestones are Berria
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clayey-calcareous sandstones and sa
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Table 17 Lithostratigraphic Units R
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11.1. Eastern Carpathians Lower Cre
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nian-Hauterivian), flysch (Barremia
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places cross-bedding is observed am
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Requienia sp. and Monopleura sp.; b
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Table 18 Zonal Schemes of the Berri
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Hauterivian sediments are represent
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Clansayesian sediments are absent a
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The Urgonian facies of the Aptian i
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Table 19 Simplified Stratigraphie S
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15. YUGOSLAVIA The Lower Cretaceous
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tain the same types of faunas. Simi
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Above the Timok Beds He the so-call
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Lower Cretaceous rocks are known fr
- Page 141 and 142:
profile El Rhoraf — Ouled Mimoun,
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In the Agadir Basin of Morocco the
- Page 145 and 146:
In the region of the Canary Islands
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To the south of the Main Caucasian
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Aar and Gotar), as well as on the s
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ammonites have been found. In the w
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In Hungary the Aptian is known in G
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and in the Aquitanian basin. The Al
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2. MAIN FEATURES IN THE EVOLUTION O
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calcareous bottom. Most characteris
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The Hauterivian marked a new stage
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U h 1 i g (1911) proposed the follo
- Page 165 and 166:
mic species during the Aptian and A
- Page 167 and 168:
Aegocrioceras and Menuticrioceras),
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(R a w s о n, 1980). The boundary
- Page 171 and 172:
subgenus Mazetoniceras, inhabiting
- Page 173 and 174:
Bathyal biotope with clayey-calcare
- Page 175 and 176:
tion from platform carbonates to th
- Page 177 and 178:
The Early Cretaceous palaeogeograph
- Page 179 and 180:
•1- г Fig. 27. Lithofacies map w
- Page 181 and 182:
of Ruse limestones deposited in the
- Page 183 and 184:
Fig. 29. Lithofacies map with sketc
- Page 185 and 186:
Fig. 30. Lithofacies map with sketc
- Page 187 and 188:
Fig. 32. Palinspastic sketch of Eas
- Page 189 and 190:
Dinaric Flysch The outer zones of t
- Page 191 and 192:
anticline), the characteristic rhyt
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The carbonates of the Moesian Platf
- Page 195 and 196:
Considerable Early Cretaceous ophio
- Page 197 and 198:
In the Apennines, Grand jacquet et
- Page 199 and 200:
Fig. 37. Palaeogeographic sketch of
- Page 201 and 202:
Fig. 40. Palaeogeographic sketch-ma
- Page 203 and 204:
Fig. 42. Palaeogeographic sketch-ma
- Page 205 and 206:
(Late Jurassic, Kimmeridgian) — t
- Page 207 and 208:
tonic evolution, at the end of the
- Page 209 and 210:
•A u b о u i n, J. 1973. Des tec
- Page 211 and 212:
В о w e n, R. 1961. Oxygen isotop
- Page 213 and 214:
Conte, G., G. Tronchetti. 1972. Etu
- Page 215 and 216:
F a u g è r e s, J. C. 1981. Evolu
- Page 217 and 218:
Kili an, W. 1887. Système Crétac
- Page 219 and 220:
К i 1 i a n, W. 1887. Système Cr
- Page 221 and 222:
N i к о I о v, T., I. S a p u n
- Page 223 and 224:
R о d i g h i e г о, A. 1919. H
- Page 225 and 226:
W i e d m a n n, J. 1964. Unterkrei
- Page 227 and 228:
Йовчева, П., Е. Трифо
- Page 229 and 230:
Пимпирев, X. 1981. Пале
- Page 231 and 232:
LE CRETACE INFERIEUR MESOGEEN (Rés
- Page 233 and 234:
Dans la marge continentale de l'Afr
- Page 235 and 236:
type néritique dans le Jura). C'es
- Page 237 and 238:
hed le Berriasien est représenté
- Page 239 and 240:
tien est présenté par des marnes
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IS. Turquie Le Crétacé inférieur
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V. EVOLUTION ET PALEOBIOGEOGRAPHIE
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2. La Province euro-caucasienne s'
- Page 247 and 248:
2. Certaines particularités du dé
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СРЕДИЗЕМНОМОРСКИЙ
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Морские нижнемелов
- Page 253 and 254:
Дофинейская зона п
- Page 255 and 256:
На размытой поверх
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до 700 m. Средний и ве
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В Юго-Восточных Род
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В ряде зон (Северна
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между двумя основн
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ным склоном почти п
- Page 267 and 268:
В раннем мелу Тетис
- Page 269 and 270:
4. Iberian Peninsula 96 4.1. Portug
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19. Proche Orient 238 Troisième pa
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ГЕОЛОГИКА БАЛКАНИК
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Fig. 1. Simplified map of the distr