THE LANGUAGE OF THE EARTH – PART VII

20
Geochronology Methods for Determining the Relative and Absolute Age of Rocks THE LANGUAGE OF THE THE LANGUAGE OF THE EARTH – PART VII EARTH – PART VII

description

THE LANGUAGE OF THE EARTH – PART VII. Geochronology Methods for Determining the Relative and Absolute Age of Rocks. Relative Age Dating - Superposition. Principles of Faunal Succession and Faunal Assemblage. Index Fossils - Widespread distribution - Restricted, known time of existence - PowerPoint PPT Presentation

Transcript of THE LANGUAGE OF THE EARTH – PART VII

Page 1: THE LANGUAGE OF THE EARTH – PART VII

GeochronologyMethods for Determining the Relative and Absolute Age of

Rocks

THE LANGUAGE OF THE THE LANGUAGE OF THE EARTH – PART VIIEARTH – PART VII

Page 2: THE LANGUAGE OF THE EARTH – PART VII

Relative Age Dating - SuperpositionRelative Age Dating - Superposition

Page 3: THE LANGUAGE OF THE EARTH – PART VII

Principles of Faunal Successionand Faunal Assemblage

Index Fossils - Widespread distribution- Restricted, known time of

existence- Common to many environments

Page 4: THE LANGUAGE OF THE EARTH – PART VII

Principle of Cross-cutting Relationships

Page 5: THE LANGUAGE OF THE EARTH – PART VII

Global Time MarkersGlobal Time MarkersVolcanic Ash Eruptions

Page 6: THE LANGUAGE OF THE EARTH – PART VII

Global Time MarkersGlobal Time MarkersMagnetic Reversals

Page 7: THE LANGUAGE OF THE EARTH – PART VII

Global Time MarkersGlobal Time MarkersMeteor Impacts

K-T impact site

K-T Boundary

coal

mudstone-impact layer

Page 8: THE LANGUAGE OF THE EARTH – PART VII

Global Time Global Time MarkersMarkers

Climate Change

Page 9: THE LANGUAGE OF THE EARTH – PART VII

Gaps in the Geological RecordGaps in the Geological RecordUnconformities

Page 10: THE LANGUAGE OF THE EARTH – PART VII

Creating Creating UnconformitiesUnconformities

Page 11: THE LANGUAGE OF THE EARTH – PART VII

Gaps in the Minnesota TimescaleGaps in the Minnesota Timescale

Page 12: THE LANGUAGE OF THE EARTH – PART VII

Regional Correlation of UnitsRegional Correlation of UnitsPiecing the Rock Record Together

Page 13: THE LANGUAGE OF THE EARTH – PART VII

Absolute Age DeterminationsAbsolute Age DeterminationsRadiometric Dating

Page 14: THE LANGUAGE OF THE EARTH – PART VII

Radioactive Isotopes

Page 15: THE LANGUAGE OF THE EARTH – PART VII

Radioactive Decay

Page 16: THE LANGUAGE OF THE EARTH – PART VII

Radioactive Decay Radioactive Decay Half-life Half-life

ZirconZrSiO4

U substitutes for Zr, but Pb does not.

Page 17: THE LANGUAGE OF THE EARTH – PART VII

87Rb 87Sr; 86Sr is stableRb – chemically substitutes for KSr – chemically substitutes for Ca

87Rb/86Sr

87Sr/86Sr

Ca-plagioclaseGranite whole rockK-feldsparBiotite (K-rich)

t=087Sr/86Sr°

t=1

Metamorphismat t=1

t=2Isochron

87Sr/86Sr°(m)

Rb-Sr Dating of a GraniteRb-Sr Dating of a Granite

Page 18: THE LANGUAGE OF THE EARTH – PART VII

GEOPUZZLE 1

Page 19: THE LANGUAGE OF THE EARTH – PART VII

GEOPUZZLE 2

Page 20: THE LANGUAGE OF THE EARTH – PART VII

GEOPUZZLE 3