Title: Divergent Plate Boundaries
1Divergent Plate Boundaries
2Global Patterns of Divergence
3Doming continental lithosphere
What Processes are Illustrated? What Geologic
Features would be Preserved?
4Processes Accompanying Doming
- Normal Faulting
- Earthquakes
- Volcanism
- What is the source of the magma?
- Based on this source, what type of volcanism
would you expect?
5The Dome Collapses Rift Valleys, Horsts,
Grabens and Half Grabens
In Addition to the Faulting and Volcanism, What
Other Processes would Operate Here? What types of
rocks would you expect?
6Additional Processes Accompanying Collapse of the
Dome
- Weathering
- Erosion
- Deposition
7Additional Processes Accompanying Collapse of the
Dome
- How much weathering would you expect in this
setting? - What would be the composition of the sediment?
- How much modification of sediment would take
place during transport? - What textures would you expect?
- What patterns of deposition would you expect?
8As Lithosphere Stretches
- Lithosphere thins
- Mafic magma is added intrusively and extrusively
- What happens to the density of the lithosphere?
- Why?
- What happens to the buoyancy of the lithosphere?
- What is the result of this?
9Lithosphere Subsides Below Sea Level
- Modern Linear Seas Red Sea, Dead Sea, Persian
Gulf - What would be the geologic record of this?
- What happens to the tectonic activity on the
edges of the continents?
10From Rifting to Drifting
- Passive Margins of Continents drift away from
axis of tectonic activity - Mid-Ocean Ridge (MOR)
- As distance from MOR increases, continental
margins cool, become more dense and subside
continental shelves - What kinds of sediments would you expect?
11From Doming to Rifting to Drifting
12Example of Rift Lithologic Association
- Mesozoic rift basins up and down the Eastern
Seaboard - Igneous and Sedimentary record in rift basins
13Evidence of Rifting Palisades Sill
14Palisades Sill lower contact
15Evidence of Relief Fanglomerates
16Evidence of Relief - Arkose
17Rift Basins Closed Drainage - Lakes