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24-Pet-A1 Principles of Stratigraphy and Sedimentation · May 2018

Question 15 of 19: Walther's Law of Facies Succession

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

Notes on this paper

EGBC National Exam — Petroleum Engineering, 17-Pet-A1 Principles of Stratigraphy & Sedimentation, 2018-May. 3 hours duration; closed book, no calculator permitted. The paper has two parts: Part A (Questions 1–10, Sedimentology and Sedimentary Processes) – Questions 1 and 2 are mandatory (10 marks each, 20 marks), plus any five of the remaining eight (3–10) at 6 marks each (30 marks), for a Part A total of 50 marks; and Part B (Questions 11–19, Stratigraphy and Sedimentary Basin Analysis) – answer any six of the nine at 5 marks each, for a Part B total of 30 marks – an 80-mark maximum (50 for Part A + 30 for Part B).

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 (sandstone/carbonate classification, diagenesis, dolomitization); Nichols, G., Sedimentology and Stratigraphy, 2nd ed., Wiley-Blackwell (fluvial/deltaic systems, sequence stratigraphy, stratigraphic units); Reading, H.G. (ed.), Sedimentary Environments: Processes, Facies and Stratigraphy, 3rd ed., Blackwell (facies models, deep-marine and shelf systems); Selley, R.C. & Sonnenberg, S., Elements of Petroleum Geology, 3rd ed., Academic Press (source rocks, basin classification, reservoir quality); International Commission on Stratigraphy, International Chronostratigraphic Chart (geological time scale).

Question 15: Walther's Law of Facies Succession (5 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.

Walther's Law (Law of Succession/Correlation of Facies, 1894) states that, in a conformable (unbroken, no significant hiatus or erosion surface) vertical succession of strata, the sequence of facies observed vertically at one location must correspond to the sequence of facies that existed laterally, side by side, across the depositional surface at any one time – only facies that were once depositionally adjacent to one another laterally can be superimposed on one another vertically without a break.

Walther's Law: lateral belts → vertical succession Lateral facies belts (time T1) Offshore mud Shoreface sand Beach sand progradation direction Vertical log (single well) Offshore mud (base) Shoreface sand Beach sand (top)
Walther's Law: as the shoreline progrades (left), a single vertical well (right) at a fixed location is buried in succession by whichever facies belt currently overlies it – the coarsening-upward vertical order (mud → shoreface → beach) exactly reproduces the lateral belt order that existed side by side at any one time.

Applicability. Walther's Law is the tool that lets a geologist reconstruct the lateral (paleogeographic) arrangement of environments from a single vertical section – essential wherever only one-dimensional data (a well, a core) is available. It is valid only across a genuinely conformable contact; any unconformity or abrupt erosional facies break severs the vertical-lateral correspondence, because non-adjacent environments can then be juxtaposed by erosion or non-deposition rather than by continuous lateral migration.