18-Geol-A3 Sedimentation and Stratigraphy · May 2016
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
EGBC National Exam — Geological Engineering, 04-Geol-A3, Sedimentation & Stratigraphy, 2016-May. Closed book, no calculator, 3 hours. Part 1 (Questions 1–12, Sedimentology and Sedimentary Processes) instructs "Answer eight questions of your choice" (8 × 5 = 40 marks) and Part 2 (Questions 13–19, Stratigraphy and Sedimentary Basin Analysis) instructs "Answer five of the following seven questions" (5 × 5 = 25 marks), for a maximum attainable grade of 65/65.
Reference texts: Nichols, Sedimentology and Stratigraphy, 2nd ed. (depositional environments, facies models, flow regime and bedforms, carbonate platforms, sequence stratigraphy, biostratigraphic correlation); Boggs, Petrology of Sedimentary Rocks, 2nd ed. (sandstone/carbonate classification, diagenesis, provenance); Selley & Sonnenberg, Elements of Petroleum Geology (turbidite reservoirs, trace-fossil facies context).
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.
Sandstones are classified along two independent axes. The first is matrix content (the Dott/Pettijohn division): a sandstone with <15% clay/silt matrix is an arenite; one with 15–75% matrix is a wacke (above 75% matrix the rock is no longer a sandstone but a mudrock). The second axis is framework composition, plotted on a Q-F-L ternary diagram with quartz (Q, including polycrystalline quartz and chert) at one apex, feldspar (F) at a second, and lithic/rock fragments (L) at the third. Within the ternary, a sandstone with >95% quartz is a quartz arenite; between 75% and 95% quartz it is a subarkose (feldspar > lithics) or sublitharenite (lithics > feldspar); below 75% quartz, with feldspar dominant over lithics, it is an arkose, and with lithics dominant over feldspar it is a litharenite. Applying the same QFL position but with 15–75% matrix gives the wacke equivalents — feldspathic wacke and lithic wacke — so the full scheme is effectively two parallel QFL triangles, one for arenites and one for wackes, selected by the matrix content.