24-Pet-A1 Principles of Stratigraphy and Sedimentation · December 2014
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
EGBC National Exam — Petroleum Engineering, 98-Pet-A1 Principles of Stratigraphy & Sedimentation, 2014-Dec. 3 hours duration; closed book, no calculator permitted. The paper has three parts: Part A1 (Questions 1–7, sedimentary processes, 5 marks each, answer any 4 of 7 for 20 marks), Part A2 (Questions 8–15, brief/multiple-choice, 3 marks each, answer any 5 of 8 for 15 marks), and Part B (Questions 16–24, stratigraphy, 5 marks each, answer any 6 of 9 for 30 marks) – a 65-mark maximum.
Reference texts: Boggs, S. Jr., Principles of Sedimentology and Stratigraphy, 5th ed., Pearson (grain texture, sediment transport, bedforms, carbonate/evaporite systems, sequence stratigraphy, unconformities, stratigraphic principles); Tucker, M.E., Sedimentary Petrology, 3rd ed., Blackwell (carbonate classification, diagenesis, dolomitization); Nichols, G., Sedimentology and Stratigraphy, 2nd ed., Wiley-Blackwell (fluvial systems, sequence stratigraphy, stratigraphic units); Reading, H.G. (ed.), Sedimentary Environments: Processes, Facies and Stratigraphy, 3rd ed., Blackwell (facies models, trace fossils); Selley, R.C. & Sonnenberg, S., Elements of Petroleum Geology, 3rd ed., Academic Press (source rocks, reservoir quality); International Commission on Stratigraphy, International Chronostratigraphic Chart (geological time scale).
Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.
Answer: (c) Cambrian → Ordovician → Silurian → Devonian → Carboniferous → Permian. This is the standard, ICS-defined order of the six Paleozoic periods from oldest to youngest, with approximate base ages: Cambrian (541 Ma) → Ordovician (485 Ma) → Silurian (444 Ma) → Devonian (419 Ma) → Carboniferous (359 Ma) → Permian (299 Ma, ending at the 252 Ma Permian–Triassic boundary). All four distractors reorder two adjacent periods relative to this sequence: (a) and (e) both place Devonian first, ahead of Cambrian; (b) swaps Devonian and Carboniferous (placing Carboniferous, the younger period, before Devonian); and (d) swaps Devonian and Silurian relative to Carboniferous. (Note: options (b) and (c) are distinct, differing in whether Devonian precedes or follows Carboniferous, and only (c) is correct.)