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Alexander Terrane

From Wikipedia, the free encyclopedia
Alexander Terrane
physiographic section
LocationAlaska; British Columbia; Yukon
Part ofWrangellia Terrane
Dimensions
  Length1,000 km (620 mi)
  Width250 km (160 mi)

The Alexander Terrane (named for the Alexander Archipelago in Alaska) is a Neoproterozoic continental fragment that originated far from its current location, before being transported and accreted to western North America in the Middle Jurassic.[1] This terrane also forms part of the composite Wrangellia Terrane.[2]

Rocks assigned to this terrane underlie much of Southeast Alaska, the north coast of British Columbia, and the Yukon southwest.[1] The Alexander Terrane is intruded by Late Jurassic and Early Cretaceous plutons and is overlain to the east by Upper Jurassic through mid-Cretaceous clastic strata and mafic volcanic rocks.[3]

In British Columbia, the terrane crops out primarily in the Coast Mountains, including the Kitimat Ranges, Chatham Sound, and Haida Gwaii, and continues to Klemtu.[1]

Origin

[edit]

The original location of the Alexander Terrane remains uncertain. Some evidence, including detrital zircon geochronology, suggests it may have formed along the margins of ancient Baltica or Laurentia,[4] however, paleomagnetic, isotopic, and fossil data indicate a possible origin near the margins of the ancient Siberian or Arctic continents.[2]

Development

[edit]

The terrane developed through three distinct phases:

Late Cambrian through Early Devonian
During the initial phase, the terrane probably evolved along a convergent plate margin.[1]
Middle Devonian through Lower Permian
The second phase is marked by strata accumulated in tectonically stable marine environments.[1]
Triassic
The third phase is marked by volcanic and sedimentary rocks which are interpreted to have formed in a rift environment.[1]

References

[edit]
  1. 1 2 3 4 5 6 Gehrels, George E.; Saleeby, Jason B. (1987). "Geologic framework, tectonic evolution, and displacement history of the Alexander Terrane". Tectonics. 6 (2): 151–173. doi:10.1029/TC006i002p00151.
  2. 1 2 Israel, Steve; Bernanek, Luke P.; Friedman, Richard M.; Crowley, James L. (2014). "New ties between the Alexander terrane and Wrangellia and implications for North America Cordilleran evolution". Lithosphere. 6 (4): 270–276. doi:10.1130/L364.1.
  3. Gehrels, G. E. (2001). "Geology of the Chatham Sound region, southeast Alaska and coastal British Columbia". Canadian Journal of Earth Sciences. 38 (11): 1579–1599. doi:10.1139/e01-040.
  4. Beranek, Luke P.; van Staal, Cees R.; McClelland, William C.; Israel, Steve; Mihalynuk, Mitch G. (2013). "Baltican crustal provenance for Cambrian–Ordovician sandstones of the Alexander Terrane, North American Cordillera: evidence from detrital zircon U–Pb geochronology and Hf isotope geochemistry". Journal of the Geological Society. 170 (1): 7–18. doi:10.1144/jgs2012-070.