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emalay516 emalay516
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6 years ago

Sandstone-carbonate-shale assemblages are characteristic of the late continental rifting phase of
  the Wilson cycle, when passive margins develop.

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PrincesskloPrincessklo
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6 years ago
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emalay516 Author
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6 years ago
Thanks for your help!!
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This helped my grade so much Perfect
ky
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2 hours ago
Just got PERFECT on my quiz
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