von Gosen W, Reinhardt L, Piepjohn K, Schmitz MD (2019)
Publication Type: Book chapter / Article in edited volumes
Publication year: 2019
Edited Volumes: Circum-Arctic Structural Events: Tectonic Evolution of the Arctic Margins and Trans-Arctic Links with Adjacent Orogens
Book Volume: 541
Pages Range: 325-348
ISBN: 9780813795416
Field studies and interpretative mapping of the area southeast of Stenkul Fiord (Ellesmere Island) revealed that the Margaret Formation clastic deposits consist of at least four sedimentary units (Units 1-4) separated by unconformities. Several centimeter-thick volcanic ash layers, identified within coal layers and preserved as crandallite group minerals (Ca-bearing goyazite), suggest an intense volcanic ash fall activity. Based on new U-Pb zircon dating (ID-TIMS) of three ash samples from one layer, this activity took place at 53.7 Ma in the early Eocene, i.e., within the period of the Eocene Thermal Maximum 2 hyperthermal. This age further suggests that the lowermost Unit 1 can be assigned to the late Paleocene-earliest Eocene, Unit 2 to the early Eocene, whereas Units 3 and 4 might be early to middle Eocene in age.
APA:
von Gosen, W., Reinhardt, L., Piepjohn, K., & Schmitz, M.D. (2019). Paleogene sedimentation and Eurekan deformation in the Stenkul Fiord area of southeastern Ellesmere Island (Canadian Arctic): Evidence for a polyphase history. In Karsten Piepjohn, Justin V. Strauss, Lutz Reinhardt, William C. McClelland (Eds.), Circum-Arctic Structural Events: Tectonic Evolution of the Arctic Margins and Trans-Arctic Links with Adjacent Orogens. (pp. 325-348).
MLA:
von Gosen, Werner, et al. "Paleogene sedimentation and Eurekan deformation in the Stenkul Fiord area of southeastern Ellesmere Island (Canadian Arctic): Evidence for a polyphase history." Circum-Arctic Structural Events: Tectonic Evolution of the Arctic Margins and Trans-Arctic Links with Adjacent Orogens. Ed. Karsten Piepjohn, Justin V. Strauss, Lutz Reinhardt, William C. McClelland, 2019. 325-348.
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