- Page 2 and 3: GEOLOGICA ULTRAIECTINA Mededelingen
- Page 4 and 5: Astronomical forcing in continental
- Page 6 and 7: Voor mijn ouders
- 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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- Page 56 and 57: 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
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Chapter 5 ' l 46 L'-value maximum t
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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
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Calvo,].P., Abdul Aziz, H., Hilgen,
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Dekkers, M.J., 1989. Magnetic prope
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Hilgen, FJ., Krijgsman, W., Raffi,
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Earth from -20 Myr to +IO Myr. Astr
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Pisias, N.G, Dauphin, J.P. and Sanc
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Shackleton, N.J., Crowhurst, S., Ha
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ecord. Rev. Ceophys. Space Phys. 15
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correspond to periods of prolonged
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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