sedimentary geology geos 240 – chapter 6 facies analysis

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Sedimentary Geology Sedimentary Geology Geos 240 – Chapter Geos 240 – Chapter 6 6 Facies Analysis Facies Analysis Dr. Tark Hamilton Dr. Tark Hamilton Readings from the Holy Book of Tark: (6:1- Readings from the Holy Book of Tark: (6:1- 26) 26) Camosun College Camosun College

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Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis. Dr. Tark Hamilton Readings from the Holy Book of Tark: (6:1-26) Camosun College. Navajo Sandstone, Jurassic Desert. Facies interpretation of Successive units in Non-Marine Sandstones A&B: trough X-beds E: Asymmetric scour - PowerPoint PPT Presentation

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Page 1: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Sedimentary Sedimentary GeologyGeology

Geos 240 – Chapter Geos 240 – Chapter 66

Facies AnalysisFacies Analysis Dr. Tark HamiltonDr. Tark Hamilton

Readings from the Holy Book of Tark: (6:1-26)Readings from the Holy Book of Tark: (6:1-26) Camosun CollegeCamosun College

Page 2: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Navajo Sandstone, Jurassic Navajo Sandstone, Jurassic DesertDesert

Page 3: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis
Page 4: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis
Page 5: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis
Page 6: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis
Page 7: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Facies interpretation of Successive units in

Non-Marine SandstonesA&B: trough X-bedsE: Asymmetric scourF: Rippled SS & MS

Page 8: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis
Page 9: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Facies interpretation of Successive units in

Non-Marine Sandstones(Left)

Planar X-bedstrough X-beds

Asymmetric scourMS

Ripple x-stratified&

Carbonates (right)Encrinal grainstonesOolite Calcarenites

Mudstones

Page 10: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis
Page 11: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Transect: Permian Reef Transect: Permian Reef MarginMargin

El Capitan, New MexicoEl Capitan, New MexicoSonnenfeld, 1993, AAPG Memoir 57Sonnenfeld, 1993, AAPG Memoir 57

Page 12: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis
Page 13: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Heirarchy ofDepositional Units& Hiatus/Diastem1)Migrating dunes2)Change inHydraulic Regime3) Lag accumulation4) Bar Migration(autogenic, 1 event)5)Channel erosion(new flood cycle)6) Allogenic:New cycle, tectonic,Eustatic, climatic

Page 14: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Nonmarine Gething FmE.K. Cadomin SandstoneBlairmore equivalent AB

(Bluesky, NEBC)

Marine Fernie Fm ShalesJurassic

Jurassic/Lower CretaceousHiatus marks regional

Tectonic Uplift across WCB

Page 15: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Adjacent environments make vertical successions

Mud Drape

RipplesLaminated silt

Planar X-beds

Trough X-beds

Erosional scour

Expansion on Gressley’s verticalSequences representing changing

Environments

Vert

ical

Lateral

Page 16: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis
Page 17: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis
Page 18: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Fining upwardsPrograding Delta

Page 19: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Waning Floods Rising Sea Level

Page 20: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

1 episode infilling

Serrated, variable hydraulics Bouma C & D or E

Page 21: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis
Page 22: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Modern Point BarsOn a meander bendIn the Milk RiverAlberta

“The present is theKey to the Past!”

Carboniferous (Penn.)Channel cut and fillWith Point Bar SandsAlabama

Page 23: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis
Page 24: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Temple of Serapis, NaplesAfter Lyell’s (1830) Geology

Marine boringslow on columns markVolcano-tectonic subsidenceFrom Vesuvio!

Re-uplift,despite rising sea levels!

A new corollary for Walther:

The Past isThe Key to the Future.Boom!

Page 25: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Destruction of SeawallVero Beach FloridaHurricane JeanneSeptember 2004

Page 26: Sedimentary Geology Geos 240 – Chapter 6 Facies Analysis

Bioturbated Ordovician Bioturbated Ordovician DolostonesDolostones

2400 km apart!2400 km apart!

a) Boothia Peninsula & b) a) Boothia Peninsula & b) Garrison QuarryGarrison Quarry

Arctic Islands versus Arctic Islands versus WinnipegWinnipeg