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JAM-2017-GG-Q1-30-explanation-upload

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Kumar Ayyasami
Presidency College, Chennai
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JAM 2017: Q 1-30-Key: 1. D. 2. B 3. B. They form in two stages. The first stage is the formation of brittle tension gashes oriented approximately 450 from the fault trend (Olson & Pollard, 1991). These tension gashes are commonly infilled with quartz or calcite. The sigmoidal shapes shown in second stage form due to rotation during ductile deformation within the shear zone. 4. C. 5. C 6. A 7. C 8. A 9. A 10. C 11. B 12. C 13. D 14. C 15. D 16. D. See dip direction and age 17. B. Dropstone is only by glacier 18. C (Phanerozoic from Cambrian to Recent) 19. A 20. A 21. D 22. A 23. B 24. B 25. A 26. C 27. D. Plagioclase is not stable in Eclogite. 28. C. 29. A 30. C

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