EESA06H3 Lecture Notes - Lecture 10: Mudstone, African Plate, Paleozoic
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How North America got built, the basic process of deconstruction, it means taking something apart and
seeing how its built and what its made out of. Thats what we're doing with continents.
We now have the tools to figure all this out, the interpreted tool is PLATE TECTONICS for understanding
how NA got built. We can do exactly the same thing with any continent, cuz basically the same process
India colliding with Asia is OBDUCTION
There are five main growth stages for NA, oldest one is called Artica (2.7 Giga annum), then Columbia
(1.8Ga), and very important one Rodinia (1.0Ga, where life evolved), the first three combined to create the
Canadian Shield (the Craton) the core of NA
Then we have the East side (Maritime Canada 350Ma, when pangea is forming, during the Appalachians
Orogeny- Appalachian Mountaints) and then the west (British Columbia-200Ma, as Pangea broke up (The
SLIDE with NA MAP, red area is the shield, blue area is appalachian belt.
Zircons (2.7bya) are used for uranium lead dating, which is a relative cheap technique that is quite precise
and can be done in large numbers. (this is one of the breakthrough methods) Tom Crowe got this technique
to the stage where it can be more easily used. (developed it), First u find the amount of lead in the crystals
using lasers and mass spectrometry and u use that to find the age. Zircon are detrital, which means they are
secondary and derived from something else, zircons originate in igneous rock and then become part of
sedimentary rock, and then metamorphosed.
Any continent that has a shield has the oldest rocks, Acasta Gneiss in Yellowknife is about 4 billion years
old. (oldest part of the NA continent) The oldest rocks are in a swiss roll pattern, continents have grown
through time by old rocks embedded in the interior. Greenland broke off about 80 million years ago and is
only separated by a failed rift.
Province is a large area defined my similar rocks and the same geology, but very sharp boundaries.
(microcontinents like India)
Origin is the rocks that result from orogenic processes, highly deformed rocks (like gneiss), (after the
continents collided, the deformed rocks that result in between like the himalayas)
1.Artica is the earliest NA landmass. 2.Nena Columbia is the second growth stage. (refer to slide), 3. then
the Grenville orogeny, (1,2 and 3 = craton), 4 and 5 are same as above.
LITHOPROBE literally means probing rocks, vehicles called dancing elephants have hydrolic plates that
are placed on the ground and exhibit very strong vibrations, it tries to mimic earthquakes by producing
seismic waves which then goes down, reflects back up by rocks of different hardness, different density,
structures, shape, and so allows us to see underground up to about 70km. The purpose was to better
understand how the canadian shield had been put together. They conducted and put together what we call a
Seismic Transects (100's in length) leads to cross sections of the shield in long distances.
Uniformitarianism means the present is the key to the past, so ancient earth behaved just like modern earth.
The earth has cooled though quite a bit since the past but its all minor stuff.
A PENE plane means almost a plane, broadly speaking the shield is flat as a result of millions of years of
erosion that literally wiped out ancient mountains. Takes about 300 million years before mountains are
completely wiped out.
The golden spike in british columbia was the last spike to build the railroad.
Obduction: the accretionary process that builds continents from smaller crustal blocks. Cratonization is the
building of cratons/shields.
A lot of ontario's mineral wealth is from the superior craton, green colored metamorphose basalts,
sometimes amphibolites, all from greenstone belt, this is because of rocks being cooked on the sea floor in
ancient times (Hydrothermal processes) Where exactly? Mid ocean ridges. Magma comes up in the mid
ocean ridges and minerals are precipitated in the rock during this process.
Pillow basalts show us that rocks formed underwater billions of years ago but have been metamorphosed,
found between blocks of continental crust, lots of gold hence the name yellowknife
Gunflint Chert is 1.1Ga and is oldest bacteria record in ontario, and simple bacteria is 3.3Ga, bacteria form
communities in stromatolites which are circular masses of bacterial colonies that are very successful, still
here today and will be here when we're gone. live in very hyper saline lagoons where there is no predators
(eg. Shark Bay)
The sudbury crater is a big depression in the surface of the shield, once thought to be volcanic, now
realized that it is a product of a huge meteorite strike. Was the second largest meteorite impact (10km in
diameter) on the planet and was big enough to go all the way through the earth's crust, largest one was
south africa. Sudbury now famous for its Nickel resources. This crater was made about 2 billion years ago.
Most craters are round, this one wasn't because its been squeezed, as southern ontario rocks got added to
north america, the grenville orogeny from 1bya. We're getting younger and younger through time
Most craters are circular but Sudbury meteorite crater is not..why?
o Its been squeezed when rocks to the south (southern Ontario) added to North America
(Grenville orogeny) about a billion years ago..deformed and squeezed
o Other lines are shield areas or fracture patterns (softer rock because it was
broken)..rocks are old
o Ice sheets have come down scoured the sheet surface
o Patent on shields
o Wanapitei Lake-young crater, 37 million yrs old (fluke)
Laurentian University in Sudbury
How north america got built, the basic process of deconstruction, it means taking something apart and seeing how its built and what its made out of. We now have the tools to figure all this out, the interpreted tool is plate tectonics for understanding how na got built. We can do exactly the same thing with any continent, cuz basically the same process everywhere. There are five main growth stages for na, oldest one is called artica (2. 7 giga annum), then columbia (1. 8ga), and very important one rodinia (1. 0ga, where life evolved), the first three combined to create the. Canadian shield (the craton) the core of na. Then we have the east side (maritime canada 350ma, when pangea is forming, during the appalachians. Orogeny- appalachian mountaints) and then the west (british columbia-200ma, as pangea broke up (the cordilleran orogeny-eg. rockies) Slide with na map, red area is the shield, blue area is appalachian belt.