SPODDS SPECIAL FIELDTRIP NEW ZEALAND, 2010 Day 3 & 4 DEEPWATER DEPOSITS OF THE LOWER MOUNT MESSENGER FORMATION, UPPER MIOCENE, TARANAKI BASIN.

Slides:



Advertisements
Similar presentations
Chapter 4 Sedimentary Structures
Advertisements

Rivers: Profiles & Landforms
Guided Notes on Erosion and Deposition
GE Sedimentary processes and products Lecture 4. Sedimentary structures II – sediment massive flows Geoff Corner Department of Geology University.
Depositional Regime of Early Triassic Sedimentation in the Bjorne Formation on the Eastern Margin of the Sverdrup Basin Ellesmere Island, Nunavut, Canada.
- The interaction of the world’s tallest building with the geology of the Basin the city is built in By Matthew Timmis and Mark Banham.
Barnett Shale Geology and Petrology SCAL, Inc. SPECIAL CORE ANALYSIS LABORATORIES, INC.
Contents Introduction Unconsolidated clastic sediments
Sedimentary Structures Clues to depositional environments.
Guided Notes About Sedimentary Rocks
UNIT 8 Surface process Biology and Geology 3. Secondary Education SEDIMENTARY BASINS.
8th Grade Science Unit 8: Changes Over Time
Sedimentary rocks Formed in seas and lakes. Formation  Rock materials  Derived from weathering and erosion  Are transported by river / wind  And later.
Sedsim modelling of controls on confined mini basin fill by eustatic and halokinetic mechanisms (Gulf of Mexico) Tristan SALLES1, Cedric GRIFFITHS1, David.
Sedimentary Rocks Sedimentary rocks are those that are formed from the collection of sediments from pre- existing rocks or through organic materials.
Horizontal and continuous beds
Unconformity. It is one of the most common geological feature found in rocks or in succession. It is different then all other geological structures viz.
Aotearoa The birth of a country.
HYDROCARBON PETROLEUM SYSTEM
S EDIMENTOLOGY AND SEQUENCE STRATIGRAPHY OF THE M IDDLE -U PPER J URASSIC K ROSSFJORD AND F ENSFJORD FORMATIONS, T ROLL F IELD, NORTHERN N ORTH S EA Richard.
Today’s Lecture:  Sedimentary structures: Inferring depositional processes from sedimentary rocks Sea-level changes & the facies concept Chapter 7: Sedimentary.
Objectives Describe how surface water can move weathered materials.
Lecture 2: Stratigraphic data Boris Natalin. Data from surface outcrops Subsurface data such as well logs, seismic data, and cores Sedimentary rocks:
GIS-based TOOL FOR REGIONAL GROUNDWATER RISK ASSESSMENT IN POORLY PRODUCTIVE AQUIFERS Janmaizatulriah JANI, David N LERNER, Steve WISE Catchment Science.
Canyons and Arches or: Why erosion is cool Angela Stickle March 5, 2007 Geology of the Desert SW.
Sculpting Earth’s Surface
Sedimentary Structures
16. Sediment Transport in the Ocean Basins – In Development William Wilcock OCEAN/ESS
Geological map of Leeds area
16. Sediment Transport across continental shelves William Wilcock OCEAN/ESS 410.
Regional Geology of Khwisero District, Kenya April 2012 Scott Patterson.
Stream Stability and Sediment Transport Environmental Hydrology Lecture 21.
Matthew Kelsch NWA Annual Meeting,18 October 2006 Hydrometeorological Training: What Makes a Flood a Flash Flood? Matt Kelsch UCAR/COMET ®
Studying Sedimentary rocks Key words fosils fossil grains Sediment Lesson objectives - To know how sedimentary rocks are formed To know that fossils are.
Definition LANDSLIDES
LITHOSTRATIGRAPHY Upper Ordovician Strata of the Appalachian Basin Utica Shale Play Book Study - Canonsburg, PA - July 14, 2015 John Hickman, Cortland.
Sedimentation of Late Pannonian clastic deposits in main and marginal basins B. Vrbanac, J. Velić & T. Malvić (Croatia) EGU General Assembly 2008, Vienna,
The Stratigraphic Record
Chapter 6 Prepared by Iggy Isiorho for Dr. Isiorho Sediments and Sedimentary Rocks Index 
Nathan D. Webb.  Background  Pennsylvanian oil production  Stratigraphy & geologic setting  Study area  Methods  Geophysical log correlation & facies.
The evolution of an elongate foreland basin: The deep- to shallow-marine filling of the Cretaceous Magallanes Basin, Chile Anne Bernhardt, Zane R. Jobe.
3D MODELING OF THE CERRO TORO DEEP-WATER AXIAL CHANNEL-BELT, SIERRA DEL TORO, MAGALLANES BASIN, CHILE: FROM OUTCROP OBSERVATIONS TO SUBSURFACE UNCERTAINTY.
Submarine Fan Depositional Processes
Bedforms in Unidirectional Flow
Major geologic terranes and belts of Massachusetts 1.
URENUI AND KIORE FORMATIONS Days 5 and 6. Field trip stops.
Stright and Bernhardt – MA-MS Calibration AAPG 2010 Sub-seismic scale lithology prediction for enhanced reservoir-quality interpretation from seismic attributes,
Submarine Fan Systems. Fining and thinning-upward or coarsening and thickening-upward successions are common in submarine fan environments Cyclicity may.
Land of lava and strata.  Gondwana land – ancient southern super- continent (break up in the early Jurassic about 184 Mya)  Great thickness of sand.
Outside! The map below shows a meandering river. Points
Revision presentation. The drainage basin 1.the edge of highland surrounding a river. 2.An area from which all precipitation flows to a single stream.
Malikah Patel1, Daniel Mikeš2
OBTAINING LOCAL PROPORTIONS FROM INVERTED SEISMIC DATA TOWARD PATTERN-BASED DOWNSCALING OF SEISMIC DATA Lisa Stright and Alexandre Boucher School of Earth.
Lecture 1: Introduction
Department of Geology and Geological Engineering
Devin R. Fitzgerald, CPG – Geologist, EMF Geoscience, Inc.
by Aitor A. Ichaso, and Robert W. Dalrymple
Label from oldest to youngest
Sedimentary Rocks.
Sedimentary Rocks!.
Welcome Back Geologists!
Modification of Rocks by Folding and Fracturing
Layer Thickness and Map Width
Department of Geology, University of Dhaka Maps and Map Reading Lab.
Geologic Maps and Cross Sections
Northern Iraq By Dr.Muhamed F. Omer
Changes in a river from source to mouth
Rivers features.
Warm-up Page: 143, 1. Igneous rock masses that form underground are called _______________. intrusions Page: 144, 2. A ____________ is a vent through which.
Presentation transcript:

SPODDS SPECIAL FIELDTRIP NEW ZEALAND, 2010 Day 3 & 4 DEEPWATER DEPOSITS OF THE LOWER MOUNT MESSENGER FORMATION, UPPER MIOCENE, TARANAKI BASIN

Content Map of the stops Outcrops Architecture Stop description Acknowledgements

Map of the stops Lower Mt Messenger Formation

Outcrops Mohakatino River Jam Roll Rapanui Stream Tongaporutu River Potroz Section (won’t be visited) Waikiekie Stream Inland section

Architecture Mohakatino RvJam Roll Potroz Packages in style of deposition Thin-bedded complex Thick-bedded sandstones MTD Siltstone package 4m Scale

Stops description Lower Mt Messenger Formation:

1. Mohakatino River Main lithofacies: Thick-bedded sandstone (S3- Ta), thickness 50 cm to 3 m Sandstone with plane lamination (Tb) and ripples (Tc) Thick bioturbated siltstone package with thin ash layers and thin sandstone beds Thin mud layers (Te) MTD Bioturbated siltstone Thin bed of bioturbated sandstone siltstone Thick-bedded sandstone Erosional contact between sandstone & siltstone

1. Mohakatino River High density turbiduty currents Energetic flows capable to erode High rate of sedimentation Small periods of time between flows

2. Jam Roll deposits Main lithofacies: Mass Transport Deposits Thick-bedded sandstones Disturbed siltstone & mudstone Courtesy of Donald Lowe

2. Jam Roll Siltstone MTD Thick-bedded sandstones Key features: Sliding blocks, soft sediment deformation Shearing surfaces Active settings Slope instabilities & failures

3. Rapanui Stream Main lithofacies: Siltstone dominated MTD Sandstone dominated MTD Thick-bedded sandstones Siltstone Sandstone with thin mudstone beds Two different MTD brought together by fault Siltstone dominated MTD Courtesy of Donald Lowe

3. Rapanui Stream Sandstone dominated MTD

4. Tongaporutu River Main lithofacies: thick-bedded amalgamated sandstone thin-bedded siltstone and sandstone highly bioturbated thick-bedded siltstone mud-clast conglomerates

4. Tongaporutu River Finninng Upward Cross-stratification in thick- bedded sandstones Key features: Overall upward fining cycle compensational style of deposition Complete cycle of Deposition

5. Inland section

6. Waikiekie stream Channels Main lithofacies: thick-bedded sandstones thin-bedded siltstone and sandstone highly bioturbated siltstone packages mud-clast conglomerates siltstone dominated MTD Key features: Nested channels Highly energetic flows Transition between lower and Upper Mt. Messenger Fm.

6. Waikiekie stream Rotated blocks Channel

18 SPODDS Students: Jon Rotzien, Lisa Stright. Zane Jobe, Katie Maier, Julie Fosdick, Anne Bernhardt, Glenn Sharman, Blair Burgreen, Acknowledgements Geological and Nuclear Sciences (GNS) in New Zealand

Thank you for your attention! New Zealand, 2009