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Paleomagnetism and geochronology of late Paleozoic granitic rocks from the Lake District of southern Chile: Implications for accretionary tectonics

Journal Article · · Geology; (USA)
; ;  [1]; ;  [2];  [3]
  1. Western Washington Univ., Bellingham (USA)
  2. Universidad de Chile, Santiago (Chile)
  3. Berkeley Geochonology Center, Berkeley, CA (USA)
K/Ar and {sup 40}Ar/{sup 39}Ar dating shows that granite rocks in the central Lake District, southern Chile, are late Paleozoic. Granitic rocks of similar age extend far up the coast of Chile, perhaps as much as 1800 km. The authors have obtained paleomagnetic directions from seven sites near Lago Ranco; these give a paleomagnetic pole at lat 57.4{degree}S, long 323.5{degree}E, with a circle of 95% confidence of 18.8{degree}. This is not significantly different from the mean late Paleozoic reference pole for the South American craton. If these results are characteristic of the late Paleozoic belt as a whole, it follows that post-late Plaeozoic accretion and terrane displacement are absent throughout much of the central Andes.
OSTI ID:
5657185
Journal Information:
Geology; (USA), Journal Name: Geology; (USA) Vol. 19:4; ISSN GLGYB; ISSN 0091-7613
Country of Publication:
United States
Language:
English