PPT-Phanerozoic Proterozoic Archean

Hadean Cenozoic Mesozoic Paleozoic Cretaceous Jurassic Triassic Quanternary Tertiary Permian Pennsylvanian Mississippian Devonian Silurian Ordovician Cambrian Phanerozoic Proterozoic. 0117 0126 0781 180 258 3600 5333 7246 1162 1382 1597 2044 2303 281 339 380 413 478 560 592 616 660 721 02 836 02 863 05 898 03 939 1005 1130 1250 1294 1329 1398 1450 1450 1521 09 1573 10 1635 10 1661 12 1683 13 1703 14 1741 10 1827 07 1908 10 , . cryptic rifting. , . potential . s. uperplumes. . and . weak plumes in the . cratonic. core. Adam . Schultz. in collaboration with. . Dhananjay. . Ravat. . , . David P . Moecher. . , . Hersh. The Phanerozoic Eons are divided by Mass Extinctions Permian How have physical changes on the earth effected the evolutionary history of life during the Phanerozoic? Types of Extinction Background Ext Lecture 1. Geologic Time Scale. From largest to smallest: Eon, Era, Period, Epoch, Age. There is also an even larger section called a supereon. However, we do not care about this one as there is only one: the Precambrian. Theda. . Strickler. , . with faculty sponsor Dr. . Chris A. . Barker, Department of Geology. ABSTRACT. STUDY AREA. Analysis of thin sections from the Wind Mountain quadrangle, Burro Mountains, NM, near the Tyrone copper mine, reveals a complex geologic history. Rock samples collected in the study area were cut using a rock saw and thin sections were prepared and analyzed to determine mineral content and fabric patterns. The oldest rocks in the study area are strongly metamorphosed and locally . 1. THE EARTH THROUGH TIME. TENTH EDITION. H A R O L D L. L E V I N. Chapter 9 . Proterozoic. : Dawn of a More Modern World. Proterozoic. Eon. 2.5 billion years to 542 million years ago. Comprises 42% of Earth history . Australia. IGG-CAS Jan. 17 2014.  Lithosphere in craton margins and adjacent orogens: seismic structure and tectonic implications . Huaiyu Yuan. Building craton lithosphere. Lee et al., . Annu. . Rev. Earth Planet. . Sample presentation created by iSpring Solutions Inc.. Cambrian . 540 to 500 mya. Ordovician . 505 to 438 mya. Silurian . 438 to 408 mya. Devonian . 408 to 360 mya. Carboniferous . 360 to 280 mya. Permian . The Geologic Column. Eonothem. Erathems. Systems. Eonothem. Erathems. Systems. Eon. Era. Periods. Chronostratigraphic. Geochronologic. Two Sets of Terminology. Precambrian. Phanerozoic. Eonothem. Robert E. Puckett Jr., Richard E. Hanson, Matthew E. Brueseke, Amy M. Eschberger Chelsea E. Toews, Joseph R. . Boro. Gravity Map with Basement Wells & Southern Oklahoma Fault System Overlay. 3D Projection of Cambrian & Proterozoic Basement Rock Geometry. by. B. Ronald Frost and Carol D. Frost. Department of Geology and Geophysics. University of Wyoming. With many thanks to J. Lawford Anderson. The Mesoproterozoic igneous event in North America occurred between 1.76 to 1.0 Ga over a distance of more than 5,000 km.. V.V. . . Shcherbakova. 1. , . Bakhmutov. V.G. 2. , . Shcherbakov. V.P. . 1. ,Zhidkov G.V. . 1. 1. Geophysical Observatory Borok IPE RAS, . Russia. . 2. Institute of Geophysics of the National. Academy of Sciences of . On the Cutting Edge – Professional Development for Geoscience Faculty . Teaching About Time Workshop. Ilyse Resnick. Premise of talk. The representation of extreme temporal magnitudes is subject to the same forces that guide our comprehension of conventional time. Geological models – “Mineral Systems”. after Kelley et al., 2006 . Supergene : regolith processes. Hypogene : source, pathway, depositional site, outflow. Contrasting physicochemical conditions.