Title Information
Title
The Rheology of Amphibolite
Name: Personal
Name Part
Getsinger, Amanda Jean
Role
Role Term: Text
creator
Origin Information
Copyright Date
2015
Physical Description
Extent
16, 180 p.
digitalOrigin
born digital
Note
Thesis (Ph.D. -- Brown University (2015)
Name: Personal
Name Part
Hirth, James
Role
Role Term: Text
Director
Name: Personal
Name Part
Cooper, Reid
Role
Role Term: Text
Reader
Name: Personal
Name Part
Fischer, Karen
Role
Role Term: Text
Reader
Name: Personal
Name Part
Tullis, Jan
Role
Role Term: Text
Reader
Name: Personal
Name Part
Stünitz, Holger
Role
Role Term: Text
Reader
Name: Corporate
Name Part
Brown University. Geological Sciences
Role
Role Term: Text
sponsor
Genre (aat)
theses
Abstract
The rheology of the lower continental crust profoundly affects our understanding of crustal dynamics, lithospheric curst/mantle coupling, and seismic hazards. However, the effect of processes associated with syntectonic hydration and metamorphism, deformation in polyphase rocks, and the evolution of a strong mineral fabric on lower crust rheology are not well constrained. To examine these processes, we conducted field and experimental investigations of deformation processes in hydrated, mafic lithologies. Field observations from a lower crust gabbro shear zone show that over ~1 meter the gabbro progresses from nominally undeformed to highly sheared where it is adjacent to a hydrous pegmatite. Phase diagrams, the presence of hydrous reaction products (amphibole), and deformation mechanism maps indicate that the water activity during deformation must have been high (~1) in the sheared gabbro compared to the non-hydrated, surrounding host gabbro. These observations indicate that fluid intrusion into mafic lower crust initiates syn-deformational, water-consuming reactions, creating a rheological contrast between wet and dry lithologies that promotes strain localization. Thus, deformation of lower continental crust can be accommodated in highly localized zones of enhanced fluid infiltration. To examine the effect of these hydration reactions on mineral fabric development and mafic rock strength, we conducted deformation experiments on powdered basalt with added water at lower crust conditions (800 ºC, 1 GPa). Amphibole formed during deformation exhibits both a strong shape preferred orientation (SPO) and lattice preferred orientation (LPO). With increasing strain, amphibole LPO rotates and strengthens with [001] maximum aligned sub-parallel to the flow direction and SPO. At low effective strain rates (10^−5 to 10^−6/s), the stress exponent is consistent with deformation accommodated by diffusion creep. The correlation of the SPO and LPO coupled with the rheological evidence for diffusion creep and progressive rotation of amphibole [001] in the direction of shear with increasing strain indicates that amphibole LPO forms via passive grain rotation. Additionally, the rheology of these amphibolites is comparable to that predicted using flow laws for wet anorthite, indicating that wet plagioclase rheology provides a good constraint on the strength of hydrated lower crust.
Subject
Topic
hydration reactions
Subject
Topic
dislocation creep
Subject
Topic
diffusion creep,continental crust
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/1096929")
Topic
Rheology
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/807961")
Topic
Amphibolite
Record Information
Record Content Source (marcorg)
RPB
Record Creation Date (encoding="iso8601")
20150601
Language
Language Term: Code (ISO639-2B)
eng
Language Term: Text
English
Identifier: DOI
10.7301/Z04J0CH3
Access Condition: rights statement (href="http://rightsstatements.org/vocab/InC/1.0/")
In Copyright
Access Condition: restriction on access
Collection is open for research.
Type of Resource (primo)
dissertations