An Isograd and Mixed-Volatile Exercise Using Data from the Ubehebe Peak Contact Aureole
Summary
This is a problem set for an introductory or advanced petrology course. It uses field data to help teach the determination and balancing of mixed-volatile reactions and locating isograds in siliceous dolomites in a contact aureole. Concepts explored in the problem set can be used to establish a framework for later discussions of T-X(CO2) diagrams, fluids in contact aureoles, and thermal gradients in the crust.
Context
Audience
This exercise is designed for a sophomore or junior level required course in petrology.
Skills and concepts that students must have mastered
How the activity is situated in the course
This is a stand-alone exercise.
Goals
Content/concepts goals for this activity
This activity helps students to better understand how to determine and balance mixed-volatile reactions and how to locate isograds in siliceous dolomite in a contact aureole.
Higher order thinking skills goals for this activity
This activity involves data analysis.
Other skills goals for this activity
Description of the activity/assignment
This is a problem set designed to be used in an introductory or advanced petrology course, either as an exercise in conjunction with a laboratory assignment or as a stand-alone assignment. It could also be easily modified to be suitable for an exam exercise. The problem set uses field data to help teach the determination and balancing mixed-volatile reactions and locating isograds in siliceous dolomites in a contact aureole. Concepts explored in the problem set can be used to establish a framework for later discussions of T-X(CO2) diagrams, fluids in contact aureoles, and thermal gradients in the crust.
Note that mapped assemblages have been somewhat simplified from the field data (Roselle 1997). Where brucite was observed in the aureole it has been mapped as periclase. All of the assemblages are '3-phase' except for the mapped assemblages of Dol+ Qtz+ Cal+ Tr. This assemblage can be the focus of a question regarding crossing tie-lines and the 'quartz-out' isograd. To simplify the exercise the open triangle symbols can be filled, making the assemblage Dol+ Cal+ Tr. Any of the questions below can be made a bit more straightforward by including more guiding text (or the reverse), depending on the preparation of the students.
The Ubehebe aureole is an excellent locality to use to teach metamorphic reactions in siliceous dolomites (Peck, 2003), and has the advantage of the availability of supplementary data for other exercises (mineral textures, Roselle, 1997; Roselle et al., 1997; stable isotopes, Roselle et al., 1999; remote sensing, Kozak et al., 2004). Ubehebe is also a case study discussed in Best's Igneous and Metamorphic Petrology (2003). Winter's (2001) textbook discusses the Alta contact aureole. A similar problem set could be easily made by using data from Alta (Cook and Bowman, 2000).
Note that mapped assemblages have been somewhat simplified from the field data (Roselle 1997). Where brucite was observed in the aureole it has been mapped as periclase. All of the assemblages are '3-phase' except for the mapped assemblages of Dol+ Qtz+ Cal+ Tr. This assemblage can be the focus of a question regarding crossing tie-lines and the 'quartz-out' isograd. To simplify the exercise the open triangle symbols can be filled, making the assemblage Dol+ Cal+ Tr. Any of the questions below can be made a bit more straightforward by including more guiding text (or the reverse), depending on the preparation of the students.
The Ubehebe aureole is an excellent locality to use to teach metamorphic reactions in siliceous dolomites (Peck, 2003), and has the advantage of the availability of supplementary data for other exercises (mineral textures, Roselle, 1997; Roselle et al., 1997; stable isotopes, Roselle et al., 1999; remote sensing, Kozak et al., 2004). Ubehebe is also a case study discussed in Best's Igneous and Metamorphic Petrology (2003). Winter's (2001) textbook discusses the Alta contact aureole. A similar problem set could be easily made by using data from Alta (Cook and Bowman, 2000).
Determining whether students have met the goals
Students have met the goals of this activity if they are able to answer the problem set completely and accurately.
More information about assessment tools and techniques.Teaching materials and tips
- Activity Description/Assignment (Microsoft Word 27kB Jan16 04)
- Instructors Notes (Microsoft Word 29kB Jan16 04)
- Solution Set (Acrobat (PDF) 287kB Jan16 04)
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Other Materials
- Regional Geology Map ( 796kB Jan16 04)
- Assemblage Map ( 1.1MB Jan16 04)
- SiO2-CaO-MgO Triangles ( 879kB Jan16 04)
- T-XCO2 Diagram ( 682kB Jan16 04)