Carlin Unconformity
The Carlin Unconformity or Carlin Trend is a linear geologic feature in northeastern Nevada which represents an old suture or collisional zone between a tectonic crustal block called a terrane and the North American Plate.
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The Carlin Unconformity or Carlin Trend is a linear geologic feature in northeastern Nevada which represents an old suture or collisional zone between a tectonic crustal block called a terrane and the North American Plate.