The Songir Structure: Inflated Lava Flow or Tube?

Authors

  • A/6 Gurudut Housing Society, Srinagar, Kalewadi Phata, Rahatani, Pune - 411 017
  • Department of Geology, University of Pune, Pune - 411 007
  • Department of Geology, Miami University, Oxford, Ohio - 45056

Abstract

A ∼9.75 km long, sinuous structure exposed near village Songir, east of Dhile has been previously interpreted to be a lava tube on the basis of remote sensing and field checks. Detailed field investigations, however, reveals an overlapping sequence of P-Type lobes and sheets, constituting a small compound pahoehoe flow, whose sinuous form has been guided by Pre-Existing topography. The Songir structure is undoubtedly a small, Sheet-Flow that propagated by repeated branching of toes and lobes that have been emplaced through the mechanism of inflation. This pahoehoe flow does not bear any resemblance to a lava tube. The study of the Songir structure reiterates the fact that greater caution should be exercised while identifying similar structures in the large and ancient Continental Flood Basalt provinces.

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Short Communications

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Published

2005-03-01

How to Cite

Duraiswami, R. A., Dole, G., & Bondre, N. (2005). The Songir Structure: Inflated Lava Flow or Tube?. Journal of Geological Society of India, 65(3), 357–365. Retrieved from http://www.geosocindia.com/index.php/jgsi/article/view/82547

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