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Transcript Table

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Course Level Date Clip# Line Interlocutor Content
- - - 1 845 TEA ∆they have the same∆ ∙hh u:h sedimentation rates initially:
- - - 1 846 UNK (0.3)
- - - 1 847 TEA and then one of the columns
- - - 1 848 UNK (0.7)
- - - 1 849 TEA u:m
- - - 1 850 UNK (0.6)
- - - 1 851 TEA °you know° maybe it's a:- it's a
- - - 1 852 TEA marine environment that suddenly gets closed ↑off→
- - - 1 853 UNK (0.6)
- - - 1 854 TEA so it's no longer receiving ∙hh maybe it's got carbonates in
- - - 1 855 TEA i:t and it's no longer building (.) a carbonate platform→ ∙hh
- - - 1 856 TEA the:n suddenly that rate of deposition has ↑changed
- - - 1 857 UNK (0.3)
- - - 1 858 TEA and you'll get this dog leg↘ you'll get a change in the slope↘
- - - 1 859 UNK (0.8)
- - - 1 860 TEA ∙hh ∇the last o:ne i:s∇ if you have a nonconformity↘ so
- - - 1 861 TEA ∇if there i:s∇ an erosional break
- - - 1 862 UNK (0.4)
- - - 1 863 TEA i:n one of the columns then
- - - 1 864 UNK (0.7)
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