Calc-alkaline%20Volcanic%20Rocks - PowerPoint PPT Presentation

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Calc-alkaline%20Volcanic%20Rocks

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Occurs as materials cool after emplacement. Hydrous minerals may decompose ... Forms due to circulation of hot ground water. Propylitic alteration ... – PowerPoint PPT presentation

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Title: Calc-alkaline%20Volcanic%20Rocks


1
Calc-alkaline Volcanic Rocks
  • Petrography
  • Processes
  • Field relations
  • Volcanic arcs
  • Petrogenesis

2
Petrography
  • Fabric
  • Classification
  • Alteration

3
Fabric
  • Aphanitic
  • Rapid cooling
  • Loss of volatiles
  • Glassy (vitric)
  • Chilling of viscous magma
  • Clastic
  • Fragmented due to rapid, violent eruption

4
Compositional Classification
  • Rhyolite
  • Rhyodacite
  • Dacite
  • Andesite
  • Latite
  • Basalt

5
Textural Classification (glassy silicic types)
  • Obsidian
  • Perlite
  • Pumice
  • Vitrophyre

6
Volcaniclastic Classification
  • Epiclastic
  • Transport by earths hydrologic system
  • Volcanic sandstone, shale, etc
  • Greywacke
  • Lahar

7
Pyroclastic Classification
  • Components
  • Vitric, crystal, lithic
  • Size
  • Ash, lapilli, blocks bombs
  • Types
  • Tuff
  • Welded tuff
  • Breccia

8
Alteration
  • Deuteric alteration
  • Occurs as materials cool after emplacement
  • Hydrous minerals may decompose
  • Due to reduction in pressure
  • Fe-Ti dusty rims on reddish pseudomorphs

9
Alteration
  • Hydrothermal alteration
  • Forms due to circulation of hot ground water
  • Propylitic alteration
  • Formation of hydrous minerals
  • Chlorite, amphibole, epidote, phrenite
  • Associated with some ore bodies

10
Extrusive Processes
  • Lava flows and domes
  • Thicker and shorter than for basalts
  • Due to higher viscosity
  • Mono Domes
  • Dacite lava flows

11
Pyroclastic Processes
  • Eruptive column
  • Pyroclastic fall
  • Pyroclastic flow
  • Pyroclastic surge

12
Ash-flow Sheets
  • Flow units
  • Cooling units
  • Welded tuffs

13
Morphology
  • Controlled by topography
  • Fill depressions
  • Even upper surface
  • Valley ponded deposits
  • Veneer deposits
  • Multiple lobes and fans
  • Lateral levees

14
Flow Unit Standard Section
  • Layer 1 (ground layer or surge)
  • Layer 2 (flow unit)
  • Layer 2a (fine-grained basal)
  • Layer 2b (main body of flow)
  • Layer 3 (ash cloud)

15
Welded Tuff
  • Degree of welding
  • Non-welded
  • Partially welded
  • Densely welded
  • Density is a good index
  • Welding (density) profiles

16
Partly Welded Bishop Tuff
Partly Welded Bishop Tuff
17
Welding Profiles
  • Density plotted vs. elevation
  • r 1.0 at base and top
  • r maximum value near center
  • Erosion easily removes upper part
  • Welding f(temperature, Pressure)

18
Vitrophyre, Armenia
19
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20
Secondary Mineralization
  • Vitrophyre
  • Devitrification
  • Lithophysae
  • Vapor-phase crystallization
  • Zeolitization

21
Compositional Zoning
  • Initial eruptions
  • Crystal-poor rhyolites
  • Crystal-rich latites or dacites
  • Related to zoned magma chambers
  • Highly-evolved upper parts
  • More primitive lower parts
  • Evidence in banded pumice

22
Calderas
  • Cauldron subsidence
  • Resurgent calderas
  • Caldera complexes
  • Origin of silicic calderas
  • Basaltic calderas
  • Active calderas

23
Collapse Calderas
  • Atitlan, Guatemala
  • Crater Lake, Oregon
  • Ksudach, Russia
  • Toya Caldera, Japan
  • Thera, Greece
  • Taupo, New Zealand

24
Caldera Characteristics
  • Simple circular form
  • Diameter gt 2 km
  • V of collapse V of tephra
  • Steep walls
  • Collapse megabreccia
  • Generally a lake

25
Model of a collapse Caldera
26
Sector Collapse Scarps
  • Horseshoe shape
  • Open towards debris apron
  • Gravitational mechanism
  • Associated with andesite cones
  • Van Bemmelen model
  • Mount St. Helens

27
Mount St. Helens, WA
28
Stages in Resurgent Calderas
  • Tumescence
  • Early rhyolite dome

29
Stages in Resurgent Calderas
  • Main events
  • Plinian fall
  • Ash flow
  • Collapse
  • Resurgent domes
  • Geothermal stage

30
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31
Origin of Silicic Caldera Complexes
  • Large calderas are only in continental crust
  • Basaltic under plating plays a role
  • Silicic magmas rise towards the surface
  • Mixed magmas are evidence
  • Marginal basaltic eruptions
  • Zoned magma chambers
  • Sequential tapping of evolving magma

32
De Silva Model
33
Large Composite Volcanoes
  • Generally polygenetic
  • Simple cones
  • Composite cones
  • Compound volcanoes
  • Volcano complexes

34
Simple Cones
  • Single summit vent
  • Small crater (lt200 m diameter)
  • Radial symmetry
  • Slopes gt 40o near summit
  • Concave profiles
  • Height of a volcano is limited
  • May grow to 3000 m
  • Mass eruption rate is a control

35
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36
Popocatepetl, Mexico
37
Continental Rifts
  • Afar example
  • Red Sea
  • Gulf of Aden
  • African rift zone
  • Mechanism
  • Extension or thermal anomaly first?

38
Convergent Zones
  • Island arcs
  • Oceanic/oceanic crust
  • Oceanic/continental crust
  • Continental margins
  • Oceanic/continental crust
  • Continent/continent collisions
  • Himalayan Mts.

39
Convergent Plate Mechanisms
  • Dipping Benioff zone
  • Earthquakes down to 600 km depth
  • Subducted slab
  • dehydrates providing rising fluids
  • heats as it goes down
  • Overlying mantle wedge
  • partially melted by rising fluids

40
Processes and Products
  • Partial melting in slab and mantle wedge
  • Fractional crystallization of magmas
  • Assimilation of crustal material
  • Formation of large magma chambers
  • calderas
  • batholiths
  • Chemically evolved products
  • Andesites and rhyolites are common

41
Arc Volcanic Petrogenesis
  • Magmas more felsic and diverse on continental
    crust
  • Suggests involvement of continental sial
  • Restricted to basalt and andesite on oceanic
    plates
  • Implies mantle derived magmas

42
Prominent Models
  • Partial melting of the lower continental crust
  • Partial melting of the subducting oceanic slab
  • Melting of Peridotite in the mantle wedge
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