Plate Tectonics on a Plane. Observations related to plate tectonics " " Plate tectonic theory types of plate boundaries!
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1 Plate Tectonics on a Plane Scripps Inst. Of Oceanography" Observations related to plate tectonics " Ocean and continent topography, hypsometry, and crustal thickness. Global seismicity, Benioff zones, and focal mechanisms Global volcanic activity Geoid Height and gravity anomaly Marine magnetic anomalies " Plate tectonic theory types of plate boundaries! Plate motions on a plane and triple junction closure" Plate motions on a sphere next lecture"!
![[Isacks, Oliver, Sykes, JGR, 1966] The theory of plate tectonics states that the lithosphere (strong layer) is divided into a small number of nearly rigid plates](/docs-images/74/70874800/images/2-0.jpg "which are sliding over the asthensophere (weak layer). Most of the deformation occurs on plate boundaries. Explain how the crust is different from the lithosphere?")
2 [Isacks, Oliver, Sykes, JGR, 1966] The theory of plate tectonics states that the lithosphere (strong layer) is divided into a small number of nearly rigid plates which are sliding over the asthensophere (weak layer). Most of the deformation occurs on plate boundaries. Explain how the crust is different from the lithosphere?
3 Study this map. There are 7 major plates and many minor plates. Memorize the names and style of the plate boundaries. Note the triple junctions. These are good questions for a quiz.
4 Assumptions: 1) Plate are only created at seafloor spreading ridges. 2) Plates are destroyed at subduction zones. 3) Plate slide past one another along transform faults. 4) The area of the Earth remains constant with time. 5) Plates can transmit stresses over global distances.
5 Spreading Ridge constructive margin Plates are created at the axis of a spreading ridge. Plates are pulled apart by tectonic forces and hot mantle material flows up to fill the gap. Melts are formed by pressure release at a depth of about 60 km. Melt accumulates into a small (magma) chamber. A ~6 km crust forms despite variations in spreading rate. The seismic layering of the crust has a sediment layer (1) above the basalt layer (2) consisting of extruded pillow basalts and sheeted dikes. These lie above a layer of gabbro (3). Spreading rates vary from 10 mm/yr to 140 mm/yr. The spreading ridge is usually perpendicular to the relative spreading vector between the plates. Of course the vector must be positive.
6 Subduction Zone destructive margin Subduction is asymmetric. The denser oceanic plate subducts under the lighter continental or oceanic plate. The negative buoyancy of the descending plate drives subduction and most plate tectonic activity. It is common for the plate to fall vertically into the mantle so the trench retreats and back-arc spreading is needed to fill the void. A volcanic arc occurs above the point where the oceanic crust reaches 150 km depth. Why? The relative velocity vector across the trench is not usually perpendicular to the trench but of course must be negative.
7 Transform Fault conservative margin Transform faults are conservative boundaries where plates are neither created nor destroyed. The sense of offset across a transform fault is either right lateral or left lateral. A Fracture zone is the inactive trace of the transform fault. The relative motion vector across a transform fault is always parallel to the spreading direction. (Next lecture we ll see that transform faults lie along a small circle about the pole of rotation between the two plates.) What is the most important TF for people living in California?
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10 SIO160 Plate Tectonics on a Plane Scripps Inst. Of Oceanography" Observations related to plate tectonics " Ocean and continent topography, hypsometry, and crustal thickness. Global seismicity, Benioff zones, and focal mechanisms Global volcanic activity Geoid Height and gravity anomaly Marine magnetic anomalies " Plate tectonic theory types of plate boundaries" Plate motions on a plane and triple junction closure! Plate motions on a sphere, see notes"!
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13 Use Google Earth to explore plate tectonics Gather the kmz files from the following ftp location for display in Google Earth. Earthquakes.kmz - Global relocated earthquakes with magnitude > 5.5 from Engdahl et al., [1997] red - shallow (0-70 km); green intermediate ( km); blue deep ( km). plate_bounderies.kmz Global plate boundaries divided into ridges, extinct ridges, trenches, and transform faults. SRTM30_PLUS.kmz Global bathymetry based on ship soundings and satellite gravity used as the base map for Google Earth. VGG.kmz Vertical gravity gradient derived from satellite altimetry used to highlight plate boundaries and fracture zones. Tectonics.kmz Digitized fracture zones and other features used to develop global plate reconstructions. age.kmz Global seafloor age based on marine magnetic anomalies and digitized fracture zones
14 Galapagos TJ
15 Galapagos TJ R R R
16 Solution to Galapagos TJ on blackboard
17 Bouvet Triple Junction
18 Bouvet Triple Junction
19 Bouvet Triple Junction R F F
20 Solution to Bouvet TJ on blackboard
21 Indian Ocean Triple Junction
22 Indian Ocean Triple Junction
23 Indian Ocean Triple Junction R R R
24 Solution to Indian Ocean TJ on blackboard
25 EXERCISE: Try all the triple junctions on this map. One could be on the quiz.
26 Plate Tectonics on a Plane Scripps Inst. Of Oceanography" What are the critical observations related to plate tectonics?" " Plate tectonic theory what are the vector rules at the three types of plate boundaries?" What is the equation for plate triple junction closure?"
ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017
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