chapter 4: igneous structures and field relationships we covered much of this in the review. a few...

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Chapter 4: Igneous Chapter 4: Igneous Structures and Field Structures and Field Relationships Relationships We covered much of this in the We covered much of this in the review. review. A few topics remain. A few topics remain.

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Page 1: Chapter 4: Igneous Structures and Field Relationships We covered much of this in the review. A few topics remain

Chapter 4: Igneous Structures Chapter 4: Igneous Structures and Field Relationshipsand Field Relationships

We covered much of this in the review.We covered much of this in the review.

A few topics remain.A few topics remain.

Page 2: Chapter 4: Igneous Structures and Field Relationships We covered much of this in the review. A few topics remain

Figure 4-1. a.Figure 4-1. a. Calculated viscosities of anhydrous silicate liquids at one atmosphere pressure, calculated by the Calculated viscosities of anhydrous silicate liquids at one atmosphere pressure, calculated by the method of Bottinga and Weill (1972) by Hess (1989), method of Bottinga and Weill (1972) by Hess (1989), Origin of Igneous Rocks. Harvard University Press. Origin of Igneous Rocks. Harvard University Press. b.b. Variation in the viscosity of basalt as it crystallizes (after Murase and McBirney, 1973), Variation in the viscosity of basalt as it crystallizes (after Murase and McBirney, 1973), Geol. Soc. Amer. Bull., Geol. Soc. Amer. Bull., 8484, , 3563-3592.3563-3592. c.c. Variation in the viscosity of rhyolite at 1000 Variation in the viscosity of rhyolite at 1000ooC with increasing HC with increasing H

22O content (after Shaw, 1965, O content (after Shaw, 1965,

Amer. J. Sci., Amer. J. Sci., 263263, 120-153, 120-153))..

Page 3: Chapter 4: Igneous Structures and Field Relationships We covered much of this in the review. A few topics remain

Structures and Field RelationshipsStructures and Field Relationships

Figure 4-5Figure 4-5. . Cross sectional structure and morphology Cross sectional structure and morphology of small explosive volcanic landforms with approximate of small explosive volcanic landforms with approximate scales. After Wohletz and Sheridan (1983), scales. After Wohletz and Sheridan (1983), Amer. J. Amer. J. SciSci, , 283283, 385-413. , 385-413.

Page 4: Chapter 4: Igneous Structures and Field Relationships We covered much of this in the review. A few topics remain

Figure 4-6Figure 4-6. . a.a. MaarMaar: Hole-in-the-Ground, Oregon (upper courtesy of : Hole-in-the-Ground, Oregon (upper courtesy of USGS, lower my own). USGS, lower my own). b.b. Tuff ringTuff ring: Diamond Head, Oahu, Hawaii : Diamond Head, Oahu, Hawaii (courtesy of Michael Garcia). (courtesy of Michael Garcia). c.c. Scoria coneScoria cone, Surtsey, Iceland, 1996 , Surtsey, Iceland, 1996 (© courtesy Bob and Barbara Decker). (© courtesy Bob and Barbara Decker).

b

c

a

Page 5: Chapter 4: Igneous Structures and Field Relationships We covered much of this in the review. A few topics remain

Figure 4-18Figure 4-18. . Types of pyroclastic flow deposits. Types of pyroclastic flow deposits. After MacDonald (1972), After MacDonald (1972), VolcanoesVolcanoes. Prentice-Hall, . Prentice-Hall, Inc., Fisher and Schminke (1984), Inc., Fisher and Schminke (1984), Pyroclastic Pyroclastic Rocks. SRocks. Springer-Verlag. Berlin. pringer-Verlag. Berlin. a.a. collapse of a collapse of a vertical explosive or plinian column that falls back to vertical explosive or plinian column that falls back to earth, and continues to travel along the ground earth, and continues to travel along the ground surface. surface. b. b. Lateral blast, such as occurred at Mt. Lateral blast, such as occurred at Mt. St. Helens in 1980. St. Helens in 1980. c.c. “Boiling-over” of a highly gas- “Boiling-over” of a highly gas-charged magma from a vent. charged magma from a vent. d.d. Gravitational Gravitational collapse of a hot dome (Fig. 4-18d). collapse of a hot dome (Fig. 4-18d).

Page 6: Chapter 4: Igneous Structures and Field Relationships We covered much of this in the review. A few topics remain

Figure 4-19Figure 4-19. . Section through a typical ignimbrite, Section through a typical ignimbrite, showing basal surge deposit, middle flow, and showing basal surge deposit, middle flow, and upper ash fall cover. Tan blocks represent upper ash fall cover. Tan blocks represent pumice, and purple represents denser lithic pumice, and purple represents denser lithic fragments. After Sparks fragments. After Sparks et al.et al. (1973) (1973) GeologyGeology, , 11, , 115-118. Geol. Soc. America115-118. Geol. Soc. America

Structures and Field Structures and Field RelationshipsRelationships

Page 7: Chapter 4: Igneous Structures and Field Relationships We covered much of this in the review. A few topics remain

Structures and Field RelationshipsStructures and Field Relationships

Figure 4-9. Development of the Crater Lake caldera. After Bacon (1988). Crater Lake National Park and Vicinity, Oregon. 1:62,500-scale topographic map. U. S. Geol. Surv. Natl. Park Series.

Page 8: Chapter 4: Igneous Structures and Field Relationships We covered much of this in the review. A few topics remain

Figure 4-23. The formation of ring dikes and cone sheets. a. Cross section of a rising pluton causing fracture and stoping of roof blocks. b. Cylindrical blocks drop into less dense magma below, resulting in ring dikes. c. Hypothetical map view of a ring dike with N-S striking country rock strata as might result from erosion to a level approximating X-Y in (b). d. Upward pressure of a pluton lifts the roof as conical blocks in this cross section. Magma follows the fractures, producing cone sheets. Original horizontal bedding plane shows offsets in the conical blocks. (a), (b), and (d) after Billings (1972), Structural Geology. Prentice-Hall, Inc. (c) after Compton (1985), Geology in the Field. © Wiley. New York.

Cracks blocks stopeCracks blocks stope

Explains structure MOR & RiftExplains structure MOR & Rift

Page 9: Chapter 4: Igneous Structures and Field Relationships We covered much of this in the review. A few topics remain

Figure 4-24. a. Map of ring dikes, Island of Mull, Scotland. After Bailey et al. (1924), Tertiary and post-tertiary geology of Mull, Loch Aline and Oban. Geol. Surv. Scot. Mull Memoir. Copyright British Geological Survey.

Page 10: Chapter 4: Igneous Structures and Field Relationships We covered much of this in the review. A few topics remain

Figure 4-26. Shapes of two concordant plutons. a. Laccolith with flat floor and arched roof. b. Lopolith intruded into a structural basin. The scale is not the same for these two plutons, a lopolith is generally much larger. © John Winter and © John Winter and Prentice Hall.Prentice Hall.

Structures and Field RelationshipsStructures and Field Relationships

Page 11: Chapter 4: Igneous Structures and Field Relationships We covered much of this in the review. A few topics remain

Figure 4-34Figure 4-34.. Diagrammatic illustration of proposed pluton emplacement mechanisms. Diagrammatic illustration of proposed pluton emplacement mechanisms. 11-- doming of roof;  doming of roof; 22-- wall rock  wall rock assimilation, partial melting, zone melting; assimilation, partial melting, zone melting; 33-- stoping;  stoping; 44-- ductile wall rock deformation and wall rock return flow;  ductile wall rock deformation and wall rock return flow; 55-- lateral  lateral wall rock displacement by faulting or folding; wall rock displacement by faulting or folding; 6-6-  (and 1)-(and 1)- emplacement into extensional environment. After Paterson  emplacement into extensional environment. After Paterson et alet al. . (1991), (1991), Contact Metamorphism. Rev. in MineralogyContact Metamorphism. Rev. in Mineralogy, , 2626, pp. 105-206. © Min. Soc. Amer., pp. 105-206. © Min. Soc. Amer.

Structures and Field RelationshipsStructures and Field Relationships