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24-Pet-B4 Well Testing · December 2015

Question 12 of 18: Define and illustrate Rimmed platform, Ramp, Sabkha, Lagoon

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

EGBC National Exam — Petroleum Engineering, 2015-Dec. 3 hours duration; closed book. This sitting's own cover page reads “98-Pet-B4, Petroleum Geology” and every question is descriptive/interpretive petroleum geology (source rocks, hydrocarbon chemistry, migration/unconventional reservoirs, carbonate traps, structural traps, Canadian basin geography) – no well-test pressure-transient content anywhere. Five (5) of the paper's six 20-mark sections are marked (NOTES item 5); all six are solved in full below so this set also serves as a complete study reference. The paper is almost entirely qualitative (draw/describe/define/list), with one true numeric calculation (Q3-2, capillary seal-breach column height).

Reference texts: Selley, R.C. & Sonnenberg, S., Elements of Petroleum Geology, 3rd ed., Academic Press (source rocks, migration, traps, carbonate systems); Tissot, B.P. & Welte, D.H., Petroleum Formation and Occurrence, 2nd ed., Springer (kerogen typing, maceral groups, catagenesis); Boggs, S. Jr., Petrology of Sedimentary Rocks, 2nd ed., Cambridge (source-rock and carbonate lithofacies); Allen, P.A. & Allen, J.R., Basin Analysis: Principles and Applications to Petroleum Play Assessment, 3rd ed., Wiley-Blackwell (structural styles, unconventional systems); Biddle, K.T. & Wielchowsky, C.C., “Trap Types in Petroleum Basins,” AAPG Memoir 60, ch.12 (structural trap classification); James, N.P. & Jones, B., Origin of Carbonate Sedimentary Rocks, Wiley-Blackwell (carbonate platform/ramp/sabkha facies models); Law, B.E. & Curtis, J.B., “Introduction to unconventional petroleum systems,” AAPG Bulletin 86 (basin-centred gas); Mossop, G.D. & Shetsen, I. (eds.), Geological Atlas of the Western Canada Sedimentary Basin, CSPG/Alberta Research Council, 1994 (WCSB stratigraphy and Canadian basin geography).

Section 4, Q4-1: Define and illustrate Rimmed platform, Ramp, Sabkha, Lagoon (8 marks)

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.

Carbonate platform geomorphology: rimmed platform, ramp, sabkha, lagoon reef rim lagoon steep slope to basin (a) Rimmed platform shoreline (high-energy shoal) deep, low-energy (b) Ramp supratidal flat (arid coast) nodular gypsum/anhydrite (c) Sabkha barrier lagoon (low-energy, restricted) open sea (d) Lagoon
Four carbonate platform-margin geomorphologies: (a) a rimmed platform, with a high-energy reef/shoal rim sheltering a low-energy lagoon behind a steep basinward slope; (b) a ramp, a gently and continuously dipping profile with no abrupt margin, high energy confined to the shoreline; (c) a sabkha, a supratidal evaporite flat with nodular gypsum/anhydrite; (d) a lagoon, a shallow, restricted water body landward of a barrier.

(a) Rimmed platform. A shallow carbonate platform with a well-defined, elevated, high-energy margin (a barrier reef or ooid/skeletal shoal complex) at the shelf edge, which shelters a lower-energy, more restricted lagoon on its landward side and drops off relatively steeply into the adjacent basin.

(b) Ramp. A shallow, low-relief carbonate depositional profile with a gentle, continuous, unbroken dip from a high-energy shoreline down into progressively deeper, lower-energy water – there is no distinct shelf-edge break in slope or barrier rim as on a rimmed platform.

(c) Sabkha. An arid, supratidal coastal (or continental salt-flat) surface above normal high-tide level where evaporative pumping of shallow groundwater/seawater precipitates evaporite minerals (gypsum, anhydrite, halite), typically as nodular or displacive textures; sabkha evaporites commonly serve as excellent top seals for underlying carbonate reservoirs.

(d) Lagoon. A shallow, semi-enclosed body of water situated landward of a protective barrier (a reef, shoal, or barrier island), characterized by lower wave/current energy, restricted circulation, and often elevated or variable salinity, favouring deposition of fine carbonate mud and, in arid settings, evaporites.