By James G. Buchanan, Peter G. Buchanan
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Additional resources for Basin inversion
_ ~ I ~ . I , I X : - ~ ~ . _-~ . . . . ~'--~ Line2585 Fig. 3. ) basin of southern Altiplano of Bolivia on faults paralleling and approximately 30 km east of the NNE-trending Uyuni-Keniani wrench fault. ~. . . . . . . . . . . . . . . . . . . . . . . . . . . . . ~-__--------------T-F-'--- 3000. Shot , I , I , I ' Points -SeismicUne 2686 ~ SOOOm-; ReflectionI ST. JOSEPH STRUCTURE Fig. 4. Seismic section (migrated) across St. Joseph structure, offshore Sabah, demonstrating inversion of mainly Middle Miocene section interpreted to have originally been deposited in a sag area.
TRICART, P. 1986. The 37 continental margin of the Mesozoic Tethys in the western Alps. Marine and Petroleum Geology, 3, 179-199. LEW~S, C. L. , GREEN, P. , CARTER, A. & HURFORD, A. J. 1992a. Elevated K/T palaeotemperatures throughout Northwest England: three kilometres of Tertiary erosion? Earth and Planetary Science Letters, 112,131-145. - - - , CARTER, A. & HURFORD, A. J. 1992b. Lowtemperature effects of the Skye Tertiary intrusions on Mesozoic sediments in the Sea of Hebrides basin. In: PARNELL, J.
A,~'~---~'~,, _ , ,OOkm ,. 100 mi. ~~r / /,~~f/Rostov-na-Dont] ....... / /,~t" 36°~ . l l k ........... _~"- .... [ ............. Basin Boundaries Fig. 1. Map showing relationship of Donbas fold belt to Dnieper-Donets basin, Ukraine. Only where fold belt crosses basin does inversion occur (Ulmishek et al. 1994, reprinted by permission). Pure Shear slip. Deep-seated transpression can convert to substantial uplift of the region above. Crust Mantle ~ Simple ~ ~ Asthenosphere £: = " ~ - ~ Shear / Sag \.
Basin inversion by James G. Buchanan, Peter G. Buchanan