“…The porphyroblasts of the L 1 lineation lie mostly within the S 1 schistosity plane that in places exhibit reverse S 1 cleavage refraction with adjacent quartzites (Eusden et al , 1996b. study of the reverse refraction relationship showed that the stiffening effects of the andalusite porphyroblasts may have rendered the pelite more viscous than the adjacent psammites during foliation development.…”
Section: Deformationmentioning
confidence: 94%
“…In 2013 we published a layperson's book, "The Geology of New Hampshire's White Mountains", which covers many aspects of the geologic history in the Presidential Range There has been excellent NEIGC fieldtrip representation for the Presidential Range over the past 21 years! An NEIGC field trip similar but not identical to this was first run by Eusden et al (1996b). led another NEIGC trip focusing on the geology from the Bronson Hill Anticlinorium east into the Central Maine Terrane south of U.S. Rte.…”
“…The porphyroblasts of the L 1 lineation lie mostly within the S 1 schistosity plane that in places exhibit reverse S 1 cleavage refraction with adjacent quartzites (Eusden et al , 1996b. study of the reverse refraction relationship showed that the stiffening effects of the andalusite porphyroblasts may have rendered the pelite more viscous than the adjacent psammites during foliation development.…”
Section: Deformationmentioning
confidence: 94%
“…In 2013 we published a layperson's book, "The Geology of New Hampshire's White Mountains", which covers many aspects of the geologic history in the Presidential Range There has been excellent NEIGC fieldtrip representation for the Presidential Range over the past 21 years! An NEIGC field trip similar but not identical to this was first run by Eusden et al (1996b). led another NEIGC trip focusing on the geology from the Bronson Hill Anticlinorium east into the Central Maine Terrane south of U.S. Rte.…”
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