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S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S Fl Fl R Fl R F C R Fl R C R R F Fl R F Fl R F Fl R R Fl R R Fl F C R R R Fl F R Fl F C R R R Fl F R Fl Fl R Fl R R Fl F Fl F Fl F R Fl F Fl F R Fl Fl R R Fl R Fl Cl R Fl F R Rs Fl F R Fl F R Fl F R Fl F R Fl R Fl Fl F R Rs Fl R Rs Fl Fl R Fl R Rs F Fl Fl Fl R Fl Fl Fl R Rs Fl R Rs Fl F Fl Fl R Fl Fl Fl R Fl A R Fl F R Fl F R Fl R Fl R Fl R F Fl R R Fl F R Rs Fl F C R Fl R Rs Fl F Rs R Rs Fl F R R Fl F R Fl S S No data III III II II II II II II II II II II II II II II II II II II II II IV I I I I IV I I IV I IV I I I I II II IV I II II II II Upper Floridan aquifer Middle semiconfining unit 1 DS AP3 DS AP2 1,070 1,075 1,145 1,130 1,120 1,115 1,110 1,080 1,085 1,090 1,095 1,100 1,105 1,125 1,135 1,140 1,150 1,155 1,160 1,165 1,170 1,175 1,180 1,185 1,190 1,195 1,265 1,250 1,240 1,235 1,230 1,200 1,205 1,210 1,215 1,220 1,225 1,245 1,255 1,260 1,270 1,275 1,280 1,285 1,290 1,295 1,300 1,305 Avon Park Formation Grain types Percent pore type m w p g f r b Grain size and texture Driller's depth, in feet below ground level Ichnofacies Trace fossils and sedimentary features frac i ii mold fene irv Ichnofabric index 1 2 3 4 5 ND m c s vfs vcs fs ms cs G P C Lost circulation zones Maximum visual est. porosity Flowmeter rate, in gallons per minute 0 147 L S Geologic unit Borehole wall image RSM HFC type Depositional sequence Hydrologic unit DE Surfaces Maximum est. permeability Flow zones Scientific Investigations Report 2017–5109 Plate 5 of 21 U.S. Department of the Interior U.S. Geological Survey Prepared in cooperation with the Broward County Environmental Planning and Community Resilience Division Detailed Graphical Lithologic Log of the Avon Park Formation in the G–2984 Test Corehole By Kevin J. Cunningham, Jared W. Kluesner, Richard L. Westcott, Edward Robinson, Cameron Walker, and Shakira A. Khan 2017 EXPLANATION Abbreviations Mudstone m Wackestone w Packstone p Grainstone g Floatstone f Rudstone r Boundstone b i Interparticle ii Intraparticle mold Particle moldic irv Irregular vug frac Fracture fene Fenestral Clay c Cobble C Mud m Silt s Very fine sand vfs Fine sand fs Medium sand ms Coarse sand cs Granule G Pebble P Very coarse sand vcs Depositional environment DE High frequency cycle HFC Relative shoreline movement RSM Not determined ND Landward L Seaward S Estimated permeability Est. perm. Estimated est. General Grain size Texture Pore type Depositional sequences Depositional sequence AP3 DS AP3 High frequency cycle type I Microbial-laminite-capped, grain-rich, peritidal cycle II Rhizolith- and mud-capped, micrite-rich peritidal cycle III Aggradational grain-rich subtidal cycle IV Glossifungites-capped subtidal cycle High frequency cycle Depositional-sequence boundary No recovery/no data Flooding surface Firmground Karst Miscellaneous symbols FS K FG FG FG FG FG K FG K FS K K K K Ichnofacies Lithofacies Porosity and permability High-energy inner shelf, shallow subtidal High-energy event, marine subtidal High-energy inner shelf, shallow subtidal Low-energy inner shelf, shallow subtidal Low-energy restricted lagoon inner shelf, subtidal Low-energy restricted inner shelf, low-energy tidal flat Low-energy restricted inner shelf, intertidal to supratidal Avon Park Formation Depositional environment (DE) Grain types, trace fossils, and sedimentary features Gastropod Ostracod Larger benthic foraminifera undifferentiated Smaller benthic foraminifera undifferentiated Planktic foraminifera Miliolid Fabularia F Fallotella Fl Coskinolina C Peloid Small echinoid Echinoid fragments Microcodium Unidentified skeletal grain Bivalve R Rotaliid Rs Reussella Amphistegina A Dasycladacean algae Rhodolith Coleiconus Cl Charophytes Intraclast B Breccia Laminae Desiccation cracks Fenestrae Planolites Burrowed mottled Thalassinoides-domintated Glossifungites firmground Psilonichnus Ophiomorpha Rhizocorallium Thalassanoides Root traces Asterosoma Grain types Trace fossils Sedimentary features S S Percent pore type Maximum estimated permeability Maximum visual estimated porosity Floatstone and rudstone Glossifungites Mudstone Skolithos Not determined Carbonate Floatstone 1–2% 0% >10–25% >2–10% >25 –50% >10–25% >1–10% >25 –50% Grainstone Cruziana Packstone Wackestone and packstone Packstone and grainstone Mudstone and wackestone Low Medium Psilonichnus Autochthonous breccia Microbial laminite 0% No Data ISSN 2328-0328 (online) https://doi.org/10.3133/sir20175109 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government This map was printed on an electronic plotter directly from digital files. Dimensional calibration may vary between electronic plotters and between X and Y directions on the same plotter, and paper may change size due to atmospheric conditions; therefore, scale and proportions may not be true on plots of this map. For sale by U.S. Geological Survey, Information Services, Box 25286, Federal Center, Denver, CO 80225, 1–888–ASK–USGS Suggested citation: Cunningham, K.J., Kluesner, J.W., Westcott, R.L., Robinson, Edward, Walker, Cameron, and Khan, S.A., 2017, Sequence stratigraphy, seismic stratigraphy, and seismic structures of the lower intermediate confining unit and most of the Floridan aquifer system, Broward County, Florida: U.S. Geological Survey Scientific Investigations Report 2017–5109, 71 p., 21 pls., https://doi.org/10.3133/sir20175109.

Depositional environment (DE) - USGS · 2017-12-07 · Kevin J. Cunningham, Jared W. Kluesner, Richard L. Westcott, Edward Robinson, Cameron Walker, and Shakira A. Khan 2017 EXPLANATION

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Page 1: Depositional environment (DE) - USGS · 2017-12-07 · Kevin J. Cunningham, Jared W. Kluesner, Richard L. Westcott, Edward Robinson, Cameron Walker, and Shakira A. Khan 2017 EXPLANATION

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1,130

1,120

1,115

1,110

1,080

1,085

1,090

1,095

1,100

1,105

1,125

1,135

1,140

1,150

1,155

1,160

1,165

1,170

1,175

1,180

1,185

1,190

1,195

1,265

1,250

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1,235

1,230

1,200

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1,210

1,215

1,220

1,225

1,245

1,255

1,260

1,270

1,275

1,280

1,285

1,290

1,295

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Percent pore type

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Scientific Investigations Report 2017–5109Plate 5 of 21

U.S. Department of the InteriorU.S. Geological Survey

Prepared in cooperation with the

Broward County Environmental Planning and Community Resilience Division

Detailed Graphical Lithologic Log of the Avon Park Formation in the G–2984 Test CoreholeBy

Kevin J. Cunningham, Jared W. Kluesner, Richard L. Westcott, Edward Robinson, Cameron Walker, and Shakira A. Khan2017

EXPLANATION

Abbreviations

Mudstonem

Wackestonew

Packstonep

Grainstoneg

Floatstonef

Rudstoner

Boundstoneb

i Interparticleii Intraparticle

mold Particle moldicirv Irregular vug

frac Fracturefene Fenestral

Clayc

CobbleC

Mudm

Silts

Very fine sandvfs

Fine sandfs

Medium sandms

Coarse sandcs

GranuleG

PebbleP

Very coarse sandvcs

Depositional environmentDEHigh frequency cycle HFCRelative shoreline movementRSMNot determinedND

LandwardL

SeawardS

Estimated permeabilityEst. perm.Estimatedest.

General Grain size Texture Pore type

Depositional sequences

Depositional sequence AP3DS AP3High frequency cycle type

I Microbial-laminite-capped, grain-rich, peritidal cycle

II Rhizolith- and mud-capped, micrite-rich peritidal cycleIII Aggradational grain-rich subtidal cycleIV Glossifungites-capped subtidal cycle

High frequency cycle

Depositional-sequence boundary

No recovery/no data

Flooding surface FirmgroundKarst

Miscellaneous symbols

FS

K

FG

FG

FG

FG

FG

K

FG

K

FS

K

K

K

K

Ichnofacies

Lithofacies

Porosity and permability

High-energy inner shelf, shallow subtidal

High-energy event, marine subtidal High-energy inner shelf, shallow subtidalLow-energy inner shelf, shallow subtidal

Low-energy restricted lagoon inner shelf, subtidal

Low-energy restricted inner shelf, low-energy tidal flat

Low-energy restricted inner shelf, intertidal to supratidal

Avon Park FormationDepositional environment (DE)

Grain types, trace fossils, and sedimentary features

Gastropod

Ostracod

Larger benthic foraminifera undifferentiated

Smaller benthic foraminifera undifferentiated

Planktic foraminifera

Miliolid

FabulariaF

FallotellaFl

CoskinolinaC

Peloid

Small echinoid

Echinoid fragments

Microcodium

Unidentified skeletal grain

Bivalve

R Rotaliid

Rs Reussella

AmphisteginaA

Dasycladacean algae

RhodolithColeiconusCl

Charophytes

Intraclast

B Breccia Laminae

Desiccation cracksFenestrae

Planolites

Burrowed mottled

Thalassinoides-domintated Glossifungites firmground

Psilonichnus

Ophiomorpha

Rhizocorallium

Thalassanoides

Root traces

Asterosoma

Grain types Trace fossils

Sedimentary features

SS

Percent pore type

Maximum estimated permeability

Maximum visual estimated porosity

Floatstone and rudstone

Glossifungites

Mudstone

Skolithos Not determined

Carbonate

Floatstone

1–2%0% >10–25%>2–10% >25 –50%

>10–25%>1–10% >25 –50%

Grainstone

Cruziana

PackstoneWackestone and packstone

Packstone and grainstone

Mudstone and wackestone

Low Medium

Psilonichnus

Autochthonous breccia

Microbial laminite

0%

No

Data

ISSN 2328-0328 (online)https://doi.org/10.3133/sir20175109

Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government

This map was printed on an electronic plotter directly from digital files. Dimensional calibration may vary between electronic plotters and between X and Y directions on the same plotter, and paper may change size due to atmospheric conditions; therefore, scale and proportions may not be true on plots of this map.

For sale by U.S. Geological Survey, Information Services, Box 25286, Federal Center, Denver, CO 80225, 1–888–ASK–USGS

Suggested citation: Cunningham, K.J., Kluesner, J.W., Westcott, R.L., Robinson, Edward, Walker, Cameron, and Khan, S.A., 2017, Sequence stratigraphy, seismic stratigraphy, and seismic structures of the lower intermediate confining unit and most of the Floridan aquifer system, Broward County, Florida: U.S. Geological Survey Scientific Investigations Report 2017–5109, 71 p., 21 pls., https://doi.org/10.3133/sir20175109.