EESA06H3 Lecture Notes - Lecture 9: Dead Oceans, Oceanic Crust, Juan De Fuca Plate

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5 Jun 2018
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Lecture 9: Canada’s Geologic Journey – The Last 4 Billion Years (Part 2)
Rodinia:
Collision zone between east coast of North America and South America Grenville
Orogeny/Grenville Orogen (crush zone that formed at that time)
o Break up and a lot of crust (Grenville Orogeny) gets left in North America
o Ontario 1 billion year ago → Geille Moutais
Goe o due to eatheig/eosio → o out  ie sheets h lots
of freshwater
Gneiss Rocks:
Formed due to pressures at really high temperature deep in the earth
These soft rocks allow plates to move
Deforming (see these bands in the gneiss) of gneiss occur as the plates move over top
o Similar to marble bread
Canadian Shield:
Covers large areas, also extends into the US and Greenland
Canadian shield is much deeper in the US
E.g., Grand Canyon have cover rocks on top that cover the Canadian shield, inner part of
canyon has gneisses
The Cambrian Explosion:
Period where first multicellular life: The Ediacara Fauna (550-500 Ma)
o Weid shaped fossils i Mistake Poit i Nefoudlad ad Walott’s Qua
Called explosion because people use to believe it was some sudden event but people
not realize it is more gradual
The Appalachian Orogeny:
Pangea forms (300 million)
Out of Africa → Maitie Caada is added
Terrane Accretion:
Terranes (silver of continental crust) are added to Eastern Canada
Eastern Canada gets built of far-travelled crust assembled during Pangea collisions
Smaller terranes can be recognized in the Appalachian Mountains
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Document Summary

Lecture 9: canada"s geologic journey the last 4 billion years (part 2) Rodinia: collision zone between east coast of north america and south america grenville. The appalachian orogeny: pangea forms (300 million, out of africa ma(cid:396)iti(cid:373)e ca(cid:374)ada is added. Terrane accretion: terranes (silver of continental crust) are added to eastern canada, eastern canada gets built of far-travelled crust assembled during pangea collisions, smaller terranes can be recognized in the appalachian mountains. Ophiolites (greek and means scaly: the remains of dead oceans, the name given to preserved ancient oceanic crust, e. g. , greenstone belts. Salt: north american in past close to equator, shallow seas evaporated (cid:271)(cid:396)i(cid:374)e (cid:894)highl(cid:455) sali(cid:374)e (cid:449)ate(cid:396)(cid:895) salt, eventually becomes salt deposits, from windsor (rock salt) The appalachian fold belt: appala(cid:272)hia(cid:374) mou(cid:374)tai(cid:374)s used to (cid:271)e talle(cid:396) (cid:271)ut (cid:374)o(cid:449) (cid:862)stu(cid:373)ps(cid:863) (cid:894)(cid:374)ot tall (cid:396)elati(cid:448)el(cid:455) (cid:455)ou(cid:374)g(cid:895), worn out, a lot of coal deposits.

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