The Orera section (Calatayud Basin, NE Spain) - Universiteit Utrecht

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GEOLOGICA ULTRAIECTINA Mededelingen van de Faculteit Aardwetenschappen Universiteit Utrecht No. 207 Astronomical forcing in continental sediments An integrated stratigraphic study of Miocene deposits from the Calatayud and Teruel basins, NE Spain Hayfaa Abdul Aziz
The investigations were supported by the Netherlands Council for Earth and Life Sciences (ALW) with financial aid from the Netherlands Organisation for Scientific Research (NWO). ISBN 90-5744-064-4
Page 4 and 5: Astronomical forcing in continental
Page 6 and 7: Voor mijn ouders
Page 8 and 9: Contents Bibliography II Introducti
Page 10 and 11: Introduction and summary During the
Page 12 and 13: common and many of these repetitive
Page 14 and 15: confirmed by magnetostratigraphy, r
Page 16 and 17: especially related to obliquity and
Page 18 and 19: Chapter [ Introduction Time control
Page 20 and 21: Chapter l and L6pez Martinez, 1985)
Page 22 and 23: Chapter T VT-III 91 90 VII 88 86 84
Page 24 and 25: Chapter 1 Overlap LY The short subs
Page 26 and 27: Chapter I Cycle hierarchy Visual ch
Page 28 and 29: Chapter [ The natural remanent magn
Page 30 and 31: Chapter I maximum unblocking temper
Page 32 and 33: Chapter I enables us to define the
Page 34 and 35: Chapter I the astronomical polarity
Page 36 and 37: Chapter [ Valdelosterreros I (VT-I)
Page 38 and 39: Chapter 2 The Orera section (Calata
Page 40 and 41: The Orera section Orera section is
Page 42 and 43: The Orera section 20 ~ 10 Om ocs I
Page 44 and 45: Chapter 3 Paleoenvironmental reCOll
Page 46 and 47: Paleoenvironmental reconstruction R
Page 48 and 49: Paleoenvironmental reconstruction (
Page 50 and 51: Paleoenvironmental reconstruction m
Page 52 and 53:
Paleoenvironmencal recon)trllction
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Paleoenvironmental reconstruction o
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Paleoenvlronn1ental reconstruction
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PaleoenvIronmental reconostruction
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Paleoenvironmental reconstruction N
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Paleoenvironmental reconstruction c
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Paleoenvironmental reconstruction 1
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Paleoenvironmental reconstruction r
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Paleoenvironmental reconstruction p
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Paleoenvironmental reconstruction r
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Paleoenvironnlental reconstruction
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Chapter 4 An astronomical polarity
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APTS for the middle Miocene ages fo
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I APTS for rhe middle Miocene Des C
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Depth domain Entire records Cycle i
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APTS for the middle Miocene The fil
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APTS for the middle Miocene saprope
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APTS for the middle M,occne L*-valu
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APTS for the middle Miocene 165 ,.,
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APTS for the middle Miocene The int
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APTS for the middle Miocene though
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Chron Lithology and cycle Stratigra
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APTS for the middle Miocene Ages of
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APTS for the middle Miocene interpr
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APTS for the middle Miocene Finally
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Chapter 5 Introduction Sedimentary
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Chapter 5 ofthe Iberian Chain and t
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Chapler 5 Canizar 25 * 20 g~~:~ _ 3
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Chapter 5 Figure 3b. indicated Phot
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Chapter 5 multierestatus, which are
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Chapter 5 above 600°C, to a maximu
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Chapter 5 80 Cascante Depth domain
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Chapter 5 Figure 6. Correlation of
Page 118 and 119:
Chapter 5 ' l 46 L'-value maximum t
Page 120 and 121:
Chapter 5 Cascante Age Model-1 9.4
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Chapter 5 points ofthe base ofC5n.r
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Chapter 5 Phase relationship The pa
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Chapter 6 One new subchron (Csr.2r-
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New subchron and cryptochrons requi
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New subchron and cryptochrons Corre
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NRM New subchron and cryptochrons (
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New subchron and cryptochrons throu
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New subchron and cryptochrons Figur
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New subchron and cryptochrons Linea
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New subchron and cryptochrons 6 (Fi
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New subchron and cryptochrons hemat
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New subchron and cryptochrons I ~g:
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New subchron and cryptochrous prefe
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References Abdul Aziz, H., Calvo, J
Page 150 and 151:
Calvo,].P., Abdul Aziz, H., Hilgen,
Page 152 and 153:
Dekkers, M.J., 1989. Magnetic prope
Page 154 and 155:
Hilgen, FJ., Krijgsman, W., Raffi,
Page 156 and 157:
Earth from -20 Myr to +IO Myr. Astr
Page 158 and 159:
Pisias, N.G, Dauphin, J.P. and Sanc
Page 160 and 161:
Shackleton, N.J., Crowhurst, S., Ha
Page 162 and 163:
ecord. Rev. Ceophys. Space Phys. 15
Page 164 and 165:
correspond to periods of prolonged
Page 166 and 167:
extending the APTS further down int
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- op basis van multidisciplinaire e
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van polariteit verwisselde heeft ge
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en In meren. Acht, gedeeltelijk ove
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In hoofdstuk 4 wordt het bewijs gel
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Acknowledgements Many (ex-)colleagu
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Curriculum Vitae Hayf;la Abdul Azi7
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The Orera section (Calatayud Basin, NE Spain) - Universiteit Utrecht

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