SH_FT - 1 ERSC 4012 El-Shazly February 12 FIELD TRIP TO...

Info iconThis preview shows pages 1–2. Sign up to view the full content.

View Full Document Right Arrow Icon
1 ERSC 4012 El-Shazly, February, 12 FIELD TRIP TO SAIH HATAT HOMEWORK PROBLEM # 5 HIGH PRESSURE METAMORPHISM IN SAIH HATAT This field trip is aimed at examining some of the high pressure, low temperature metamorphic rocks which occur in the Saih Hatat area (structurally underlying the Semail ophiolite), and at illustrating some of the deformational and metamorphic events that predated or were contemporaneous with the Semail ophiolite emplacement. High pressure, low temperature (high P/T) metasediments from this area were first reported by Michard et al. (1982). Blueschists were then described by Lippard (1983). More detailed petrologic studies by Le Métour et al. (1986), Goffé et al. (1988), El- Shazly et al. (1990) and El-Shazly and Liou (1991), Searle et al. (1994) have led to the proposition of several tectonic models for the area (e.g. Lippard et al., 1986; Le Métour et al., 1990; El-Shazly and Coleman, 1990; El-Shazly and Lanphere (1992), El-Shazly (1994)). Keep in mind that all these models are controversial, and that the relationship between deformation and metamorphism remains poorly understood. Following this field trip, you are supposed to write a short essay (3-5 pages long) on high pressure metamorphism in Saih Hatat. The questions on this handout are designed to help you write this essay, so be sure to have them all answered before you leave each stop! In this essay, you should point out the different mineral assemblages occurring in rocks of different bulk compositions that you have seen, the tectonostratigraphic positions of these units or rock types and the directions of increase in metamorphic grade throughout Saih Hatat (detected by mineralogical changes in rocks of the same composition). Afterwards, you should: 1- plot the different mineral assemblages on Figs. 1 and 2 2- identify the "index minerals" characteristic of certain rock types in each area, and label what you think may be metamorphic zones accordingly. How do your metamorphic zones compare with those of Le Métour et al. (1990), shown on Fig. 3? 3- Prepare a paragenetic sequence diagram for metapelites in all of your metamorphic zones (similar to the one shown on the last page of this handout, copied from Le Métour et al. (1990) for metabasites). 4- Based on field relations, you should then critique one or two of the tectonic models mentioned above, keeping in mind that you do not have to agree with any of these models! Use the papers cited above to your advantage! Introduction:
Background image of page 1

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Image of page 2
This is the end of the preview. Sign up to access the rest of the document.

This note was uploaded on 02/28/2012 for the course GLY 421 taught by Professor Staff during the Fall '11 term at Marshall.

Page1 / 4

SH_FT - 1 ERSC 4012 El-Shazly February 12 FIELD TRIP TO...

This preview shows document pages 1 - 2. Sign up to view the full document.

View Full Document Right Arrow Icon
Ask a homework question - tutors are online