Transcript Table
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Results of Search: 176,291 lines — Showing 77601 - 77620.
| Course | Level | Date | Clip# | Line | Interlocutor | Content |
|---|---|---|---|---|---|---|
| - | - | - | 1 | 88 | TEA | your clasts↘ a:nd |
| - | - | - | 1 | 89 | UNK | (0.5) |
| - | - | - | 1 | 90 | TEA | what are the relative sizes of tho:se- |
| - | - | - | 1 | 91 | UNK | (0.2) |
| - | - | - | 1 | 92 | TEA | of the matrix and the clasts↘ so: |
| - | - | - | 1 | 93 | UNK | (1.0) |
| - | - | - | 1 | 94 | TEA | u:h you need to ∆include that information∆ |
| - | - | - | 1 | 95 | TEA | as ↑well a:s ∙hh is the matrix mostly ↑quartz↘ |
| - | - | - | 1 | 96 | TEA | is it a fine grain quartz↗ is it ∙hh u::h |
| - | - | - | 1 | 97 | UNK | (0.2) |
| - | - | - | 1 | 98 | TEA | is it a cla:y↗ is it a mudstone↗ are your |
| - | - | - | 1 | 99 | TEA | cla:sts ↑quartz→ are they feldspar→ because ∙hh tha:t |
| - | - | - | 1 | 100 | TEA | u:h information changes your interpretation of the rock↘ |
| - | - | - | 1 | 101 | TEA | hh ∙hhh so if you lo:st (.) points for tha:t |
| - | - | - | 1 | 102 | UNK | (0.5) |
| - | - | - | 1 | 103 | TEA | that's why i think that i: ∙hh have been pretty thorou:gh |
| - | - | - | 1 | 104 | TEA | in my: notes→ |
| - | - | - | 1 | 105 | UNK | (1.0) |
| - | - | - | 1 | 106 | TEA | u:hm additionally→ |
| - | - | - | 1 | 107 | UNK | (0.2) |