File:M106Ch04Fig2A.jpg
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Paleogeographic maps of Libya. (A) Pan-African structures that formed during late Precambrian to Late Carboniferous tectonism. (B) Hercynian structural trends caused by the Late Carboniferous collision between Gondwana and Laurasia. Sources: Klitzsch (1971), Zegaar (1986), Anketell (1996), and Hallett (2002) 500 km (310.7 mi). From Hassan, H. S., and C. C. G. Kendall, 2014, Hydrocarbon provinces of Libya: A petroleum system study, in L. Marlow, C. Kendall, and L. Yose, eds., Petroleum systems of the Tethyan region: AAPG Memoir 106, p. 11-141.
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 19:44, 28 March 2016 | | 700 × 633 (66 KB) | Molyneux (talk | contribs) | Paleogeographic maps of Libya. (A) Pan-African structures that formed during late Precambrian to Late Carboniferous tectonism. (B) Hercynian structural trends caused by the Late Carboniferous collision between Gondwana and Laurasia. Sources: Klitzsch (... |
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