EDITORS: A color slide of a limestone deposit sampled in the U-M study is available on request.
ANN ARBOR---When continental plates come together to form mountain ranges, the impact from the collision bends microscopic grains in rocks more than 1,200 miles away, according to an article published in this week's issue of Science.
"Classic plate tectonics theory maintains that all activity is concentrated at the plate margins, but our evidence shows that seemingly quiet mid-continent areas are highly sensitive recorders of plate tectonic activity," said Ben A. van der Pluijm, University of Michigan professor of geological sciences.
When examined under a microscope, calcite grains in limestone samples, collected by van der Pluijm and his colleagues at more than 70 North American mid-continental locations, all showed the characteristic bending or deformation pattern produced in rocks under shearing stress. Intensities of stress recorded in the limestone samples varied directly with distance from the Appalachian and Rocky Mountain ranges.
"These grains of calcite are like stress gauges placed in the Earth long ago," said van der Pluijm. "Since each deformation pattern corresponds to a specific stress level and orientation, these patterns preserve a permanent record of the effects of plate collision and mountain-building over long periods of geologic time." Published in the Aug. 8 issue of Science, the research was conducted by van der Pluijm; John Craddock, associate professor of geology at Macalester College; U-M undergraduate student Brita Graham and U-M graduate student John H. Harris.
Stresses in continental plate interiors---a region long ignored by geologists---could provide new insights on tectonic processes, such as basin formation and fault reactivation, and offer critical input for computer modeling of plate dynamics, according to van der Pluijm.
U-M researchers collected samples from limestone deposited between 500 million and 200 million years ago---a period of time when the North American mid-continent often was covered with shallow seas. Samples were taken at regular intervals along two transects or straight lines. One sampling line extended from the Rocky Mountains in Wyoming into Minnesota. The second line, which replicated results from a previous study, originated in the Appalachian Mountain range in Tennessee and extended into Indiana.
"Surprisingly, deformation patterns from both transects were identical, even though the Appalachian range on the eastern side of the North American continent differs dramatically in age and style of mountain formation from the Cordilleran range on the western side," van der Pluijm said. "Mountain belts appear to act as 'stress filters' absorbing any variations in plate margin conditions before transmitting stress into plate interiors."
While the orientation of the calcite grain stress indicators did not change along either transect, the level of stress recorded decreased steadily with distance from the mountain range. Stress levels recorded in Wyoming nearest the Rockies, for example, were about five times greater than those recorded in western Minnesota.
"Our data show that mid-continent areas are not quiet and tectonically dead, as geologists believed," van der Pluijm said. "Transmitted stresses were associated with a host of geologic phenomena, including motion and earthquakes along ancient faults created long before recent mountain-building occurred."
The research project was funded by the Pew Charitable Trust, the Blandin Foundation, the Huron Mountain Wildlife Foundation and the National Science Foundation. U-M senior Brita Graham participated in the project through the U-M College of Literature, Science, and the Arts' Undergraduate Research Opportunity Program, which facilitates undergraduate involvement in faculty research.
The above post is reprinted from materials provided by University Of Michigan. Note: Materials may be edited for content and length.
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