400 likes | 1.15k Views
Geology 3120 - Sedimentary Structures. Outline. Review the geologic history exercise from last time Contacts, primary structures, and secondary structures How to determine which “way is up”… Cross-bedding, graded-bedding, reverse graded-bedding
E N D
Outline • Review the geologic history exercise from last time • Contacts, primary structures, and secondary structures • How to determine which “way is up”… • Cross-bedding, graded-bedding, reverse graded-bedding • Determining way up using top surface features - ripples, mudcracks, raindrops, footprints • Determining way up using bottom surface features - load casts • Determining way up using features within rocks - geopetal, bioturbation, stromatolites, flame structures, pillow lavas
Geologic History • 12 Ma dike • 15 Ma dike • Normal fault • 20 Ma sed • 22 Ma sed • Erosion • Thrust fault • Folding • Layer B • 60 Ma sed • Layer G • 70 Ma sed • 80 Ma sed
Contacts, Primary Structures & Secondary Structures • Contact - a boundary between rock units • Primary structure - structures that form during lithification • Secondary structure - structures that form after lithificaiton
Contacts, Primary Structures & Secondary Structures • Contact - a boundary between rock units • Primary structure - structures that form during lithification • Secondary structure - structures that form after lithificaiton
Which way is up? Today Option 1 Overturned syncline Option 2 “up side down” overturned anticline
Cross-bedding Checkerboard Mesa, Zion National Park Younger Flow direction Y Concave up Older
Graded bedding Younger Y Older • Decrease in depositional energy with sedimentation • Example: flood deposits, turbidity currents
Graded bedding Younger Y Older • Decrease in depositional energy with sedimentation • Example: flood deposits, turbidity currents
Reverse (Inverse) Graded Bedding Younger Y Older • Increase in depositional energy with sedimentation • Example: debris flows (a lot less common than normal graded beds)
Ripple marks Y • Symmetric ripples indicate bi-modal current • Concave = up • Asymmetric ripples indicate unidirectional current
Mud cracks • Desiccation of muddy sediments • Mud cracks 5 cm
Raindrops Y • Limited to terrestrial sediments
Footprints Y • Limited to terrestrial sediments
Load casts • Protrusion of material into a layer below • Load casts indicate the base of a layer, not the top of a layer • Determining the current direction may be possible
Geopetal Structures Y • A “natural” carpenter’s level Shell or cavity in the rock Matrix Infill material (I.e., calcite)
Y Bioturbation • Habitation burrows • Feeding burrows • Movement
Stromatolites Y • Sharks Bay, Australia • Cyanobacteria grow upward toward the surface
Flame structures Y • Less dense material intrudes into material above • Caused by rapid loading of turbidite sands
Pillow lava Y Upper curved surface “V “ notch
References Slide 8 http://www.utahpictures.com/Checkerboard.html Slides 9-15, 17 Busch, R. M. and D. Tasa, Laboratory Manual in Physical Geology, 3rd. Ed., American Geological Institute and National Association of Geology Teachers, 260 p., 1990. Slide 18 http://www.discoverwest.com.au/hablin.html Slide 20 http://volcanoes.usgs.gov/Products/Pglossary/PillowLava.html http://volcanoes.usgs.gov/Products/Pglossary/ancientseq.html