RGE-PGS Vercors-Nyons field course
IFP School
Created on September 22, 2020
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Transcript
RGE-PGS 2020-21
Vercors & Southeast basinField course
October 3 - 9, 2020
Teachers: A. Torres, J-P. Roy
Videos: O. Lerat
Please report bugs- if any
Start
South Vercors uplands and Southeast basinField course outcrops & stops summary
Introduction
Day #1
Day #2
Day #3
Day #4
Day #5
Day #6Wrap up
Objectives:A multi-scale geological analysis on various outcrops in the Southeastern part of France:
- to illustrate the relationship between shelf and basin, via the observation of typical depositional environments:
- to illustrate the variety of depositional facies and processes in shallow marine, littoral and coastal environments.
INTRO - page 2/4
Introduction toVercors-Nyons field course
Vercors uplands (area 1)Southeast basin (area 2)outcrops
A multi-scale geological analysis on various selected outcrops in the Southeastern part of France - Vercors uplands and Southeast Valréas basin: 1) Illustrate the relationship between a shelf (carbonate and siliciclastic) and its related basin, via the observation of typical depositional environments: - platform carbonate facies (Urgonian) - gravity-driven shelfal and slope sand bodies - basinal sedimentation: gravitational processes (slope and basin: feeding & by-pass channels, slumps, MTD, deep-sea fans: channels & lobes,...) and pelagic decantation (black shales/marlstones as potential source rocks) 2) Illustrate the variety of depositional facies and related processes in shallow marine, littoral and coastal environments (tidal-dominated, wave-dominated, Gilbert delta, lacustrine deposits, incised valleys,...) 3) Evaluate potential reservoirs geometry and quality4) Place all observations in a global geological context (i.e. relationship between tectonics and sedimentation: Alpine orogeny tectonic cycle) and illustrated with paleogeographic reconstructions
INTRO - page 1/5
D1
INTRO
D2
D3
D4
D5
D6WRAPUP
Geological map of Southeastern France
MassifCentral
MassifAlpin
Google Earth geological map of France
To download the geological map of France: 1. go to Google Earth 2. Download the kml file 3. Upload it into Google Earth "Projects" 4. Tick the file to visualize it as an overlay on the satellite base map
INTRO - page 2/5
Download "InfoGeol" smartphone app from BRGMInfoTerre
D1
INTRO
D2
D3
D4
D5
WRAPUP
Google Earth map
Google Earth
Google Maps
Area 1
Area 2
Stops and outcrops locations:
INTRO - page 3/5
D1
INTRO
D2
D3
D4
D5
WRAPUP
To load the map: 1. go to Google Earth https://earth.google.com/web/ 2. Download the kmz file 3. Upload it into Google Earth
To load stops locations: 1. go to Google Earth https://earth.google.com/web/ 2. Download the kmz file 3. Upload it into Google Earth
Area 1: South Vercors uplands (Diois: Die area)
INTRO - page 4/5
D1
INTRO
D2
D3
D4
D5
WRAPUP
Area 2: Southeast basin (Valreas sub-basin)
BassindeValréas
Geological map of Valence area
INTRO - page 5/5
Topographic map of the Baronnies provençales area
Geological evolution of the Baronnies(flyer in French)
D1
INTRO
D2
D3
D4
D5
WRAPUP
Day #1Vercors carbonate platform(Area 1)
Stop#1 - La Montagnette
(Landscape view from "cabane de 'lEssaure" sheepfold , 1647m) Prograding Barremian-Aptian carbonate platform. Shelf-break clinoforms geometry due to sea level variations.
(Landscape view from Bénevise northern entrance) Carbonate shelf-break clinoforms organization in response to eustatic cycles.
(Roadcut in curve) Deep-sea channel cut through thick pelagic carbonate series.
Stop#2 - Rocher de Combau
Stop#3 - Cirque d'Archiane
D1
INTRO
D2
D3
DAY1 - page 1/2
D4
The Urgonian limestone is a sedimentary facies from the Lower Cretaceous, corresponding to the Aptian and Barremian stages, very abundant in the subalpine ranges (Vercors, Chartreuse massif) and south-eastern France. This facies corresponds to a reefal bioclastic grainstone, built in a shallow sea, in a tropical climate.It is characterized by its very light color, often white. Its strength and white color make it a stone widely used in building. Its name comes from the town of Orgon.
D5
WRAPUP
Stop#3 - Cirque d'Archiane
D1
INTRO
D2
D3
D4
D5
WRAPUP
Day #1 (day 6)
Stop#1 - La Montagnette
Stop#2 - Rocher de Combau
Carbonate shelves
RetrogradationProgradation
Mallorca reef(Kendall)
Landscape scenery
DAY1 - page 2/2
Channel fill
La Montagnette in fog & snow
Day #2 Deep-sea carbonate & clastic series(Area 2)
D1
INTRO
D2
D3
D4
D5
WRAPUP
Stop#4 - L'Eyzarette
(Roubion meander roadcut)Upper Barremian deep-sea carbonate series: mudstones/marls, and turbidite cut by a by-pass channel.
(Liotoir gully)Aptian pelagic shales, slumps incised by large turbidite channel.
(Roadcut) Aptian turbidite channels with injectite facies in sandstone.
Stop#5 - Les Cosmes
Stop#6 - Crupies
DAY2 - page 1/2
Day #2 (day 7)
D1
INTRO
D2
D3
D4
D5
WRAPUP
Stop#4 - L'Eyzarette
Stop#5 - Les Cosmes
Stop#6 - Crupies
Architecture of a deep-sea fan
(Reading & Bowman, 1998)
Turbidite channels
Gravity-driven transport processes (Shanmugam et al., 1995)
Flume-tank turbidite
Erosional channel base (mudclasts)
DAY2 - page 2/2
Injectite facies in glauconitic sandstone
Deep-sea architectural elements (SEPM)
MTDs
(Posamentier et al., 2011)
Erosionalfeature
Carbonate turbidite channels
day #3 Baronnies SLOPE & BASIN carbonate & clastic series
D1
INTRO
D2
D3
D4
Stop#7 - Col de Palluel
D5
(Outcrop on raod side)Basin pelagic deposits (Aptian-Albian black shales): potential source rock. After 55 My of deep sedimentation, erosion of ~1000m.
WRAPUP
(Cliff across Blême river)Low-density turbidite distal lobes (late Aptian). Typical Bouma sequence in clean sandstone with abundant flow-generated bedforms and dewatering features.
Stop#8 - Serre d'Autruy
Stop#9 - L'Épine
(Roadcut close to Montclus) "Slumporama". Severe slope instability (alpine tectonics) in Barremian limestones.
(Large rocky plateau) Megaturbidite (Albian): massive sand body with injectites (dykes & sills). "Pumpkin balls" diagenetic cementation facies and polygonal contraction fracture network.
Stop#10 - Brunet
DAY3 - page 1/2
Rain...
Rain...
Day #3
D1
INTRO
D2
D3
D4
D5
WRAPUP
Stop#10 -Montclus(Brunet)
Stop#7 - Col de Palluel
Stop#8 - Serre d'Autruy
Stop#9 - L'Épine
Deep marine “background” sedimentation
DAY3 - page 2/2
Barremian rhapsody (slumporama)
Partial Bouma sequence in distal lobes
Day #3 (day 8)
day #4Mesozoic shelf & Cenozoic shallow marine series
D1
INTRO
D2
D3
Stop#11 - Tour d'Alençon
D4
D5
(Outcrop close to the castle tower) Albian shelf megaripples and dunes built by deep longshore currents - source of deep-marine turbiditic system.
(Landscape view from crossroad) Structural interpretation and hand sketch of La Lance anticline closure (Mont Rachas).
(Roadcut facing bridge over Lez river) Fractured potential carbonate reservoir (Turonian). Statistical fracture distribution analysis for preferential drains prediction.
WRAPUP
Stop#12 - Béconne
Stop#13 - Montjoux
DAY4 - page 1/2
Special thanks to Imoleayo for the backup videos!
Cretaceous/Miocene unconformityEastern edge (La Lance Western flank) of the basin. Numerous tidal features.
Stop#14 - Venterol
(windy...)
Day #4 (day 9)
D1
INTRO
D2
D3
D4
D5
WRAPUP
Stop#11 - Tour d'Alençon
Stop#12 - Béconne
Stop#14 - Venterol
Thin section in clean Albian poorly consilidated, galuconitic sandstone
Stop#13 - Montjoux
13
12
Burrowed Turonian limestone
<- Remember Sylvie's course...
DAY4 - page 2/2
Wavy laminations in tidal sandstone (Langhian)
- - - 70 My unconformity - - -
Shark teeth indune sandstone
day #5Cenozoic shoreface & continental series
D1
INTRO
D2
D3
Stop#15 - Calvary
D4
D5
(Roadcut)Tidal shoreface deposits & small channel with bioclasts (Serravallian: "Valréas sandstone").
(Outcrop on hill) Storm deposits (Serravallian) in wave-dominated shoreface environment (HCS) incised by a tidal channel with large cross-stratifications and "herringbones".
WRAPUP
(Former quarry)Miocene (Tortonian) fluvial conglomerates (Gilbert delta) deposited in shallow tidal shoreface environment.
Stop#16 - La Garenne
Stop#17 - Le Serre
Stop#18 - La Castanière
(Vineyard meadow)Lacustrine marls rich in black OM, lacustrine mudstone and fluvial conglomerate (Tortonian) with erosional base.
(Cliff in gully)Pliocene (Chabrier) conglomerates (Gilbert delta) in shallow tidal shoreface.
Stop#19 - Les Lintils
DAY5 - page 1/2
Trough cross-bedding
Day #5 (day 10)
D1
INTRO
D2
D3
D4
D5
WRAPUP
Stops#15, 16, 17, 18 & 19
Lithological log and structural cross-section construction of Nyons area.
Clastic system tracts (Kendall)Formation of incised valleys
DAY5 - page 2/2
Gilbert delta
The Messiniancrisis
day #6field course wrap up
D1
INTRO
D2
D3
D4
D5
(Landscape view on La Lance anticline and Nyons basin)
D6WRAPUP
Stop#20 - Saint Rimbert
General panorama of "La Lance" Mesozoic anticline and of Valreas Cenozoic basin (Nyons: eastern edge).
WRAP UP - page 1/2
Pictures!
Last picnic lunchin the field...
ThePontiaswindlegend...
About climate change - Zachos, 2008
Milanković cycles
Please add yours - especially group and outcrop ones. Thanks!
With or without...
[Available until Dec. 31, 2020 only...]
day #6field course wrap up
D1
INTRO
D2
D3
D4
D5
(Landscape view on La Lance anticline and Nyons basin)
D6WRAPUP
Stop#20 - Saint Rimbert
General panorama of "La Lance" Mesozoic anticline and of Valreas Cenozoic basin (Nyons: eastern edge).
WRAP UP - page 1/2
Pictures!
Last picnic lunchin the field...
ThePontiaswindlegend...
About climate change - Zachos, 2008
Milanković cycles
Please add yours - especially group and outcrop ones. Thanks!
With or without...
[Available until Dec. 31, 2020 only...]
D1
INTRO
D2
D3
D4
D5
D6WRAPUP
Field course report subjects 1. Hydrodynamic processes controlling the deposition of potential reservoirs along a passive margin - from field examples: Southeast Basin, Somme river bay. Groups: 3 & 8 2. Deep-marine deposits / turbidites: gravity processes: facies and reservoir potential. Groups: 5 & 11 3. Reservoir architecture in wave-dominated environment: shoreface facies – theory and field examples. Groups: 2 & 6 4. Sedimentology of reservoirs in tidal-dominated environment – theory and field examples. Groups: 10 & 12 5. Incised valleys: formation and filling; related potential reservoirs facies distribution and geometry. Groups: 4 & 7 6. Tectonic influences on sedimentation: Valreas basin evolution and development of related reservoirs. Groups: 1 & 9 Report format“GEOLOGY” paper (title, length, font size,…) GSA (www.gsapubs.org)- 4 pages (maximum - i.e. 3000 words) of text: Abstract / Introduction / Discussion / Conclusion + References (if any) – 4 points for each + 4 points for document presentation/appearance (general organization, clarity, concision, care/attention). - 4 pages (maximum) of appendices / figures / pictures (quality and relevance with relation to text and topic) All reports will eventually be compiled in a single collective document of which each student will get a personal copy. Deadline: Nov. 6th, 2020
Day #6: additional documents
WRAP UP - page 2/2
Watch
Debris flows
Turbidite flows transformation
Structural & stratigraphic evolution
Bedload transport and bedforms
Gravity deposits
PPT presentations
Geological map
(Refer to PPTs)
(Refer to videos)