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1 edition of A stratigraphic section through the Silurian turbidite sequence (Peary Land Group) in northern Nyeboe Land, north Greenland. by Poul-Henrik Larsen and Jan C. Escher found in the catalog.

A stratigraphic section through the Silurian turbidite sequence (Peary Land Group) in northern Nyeboe Land, north Greenland. by Poul-Henrik Larsen and Jan C. Escher

A stratigraphic section through the Silurian turbidite sequence (Peary Land Group) in northern Nyeboe Land, north Greenland. by Poul-Henrik Larsen and Jan C. Escher

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Published by Geological Survey of Greenland in Copenhagen .
Written in English

    Subjects:
  • Geology - Greenland

  • Edition Notes

    11

    The Physical Object
    Pagination21 p.
    Number of Pages21
    ID Numbers
    Open LibraryOL21992662M

    A turbidite is a sedimentary bed deposited by a turbidity current or turbidity flow. It is composed of layered particles that grade upward from coarser to finer sizes and ideally display a (complete or incomplete) Bouma sequence (Bouma, ).Mud-dominated turbidites (fine-grained turbidites) may show the sequence detailed by Stow and Shanmugam ().   This contribution concerns a structural transect through the Silurian rocks of the Fredericton Belt up to the Fredericton Fault (Fig. 2). The transect runs from Longs Creek, 20 km west of Fredericton, to Deerwood Drive, 5 km southwest of the city (Fig. 2), and includes a 3 km across-strike section through the Silurian Kingsclear Group up to the.

    the generation of a robust sequence stratigraphy model that accounts for the characterization of the turbidites found in the F3 Block North Sea prograding Tertiary delta complex. Data and Methodology. The principal data of this study is a high-quality 3D PSTM from the block F3, located in the North Sea Offshore of Netherlands. A notable circumstance of late Early through Late Silurian sedimentation on the Great Lakes area craton is that at least two and possibly three cycles of third-order duration (if eustatically considered) are recognized in basin and shallow-platform settings alike. Both virtually pure and siliciclastic-rich carbonate rocks exist in parts of platform-situated sections in contrast to.

    Silurian (Depth m, thickness m) The Silurian section is composed of sandstone, siltstone, shale, and barren of fossils. The sandstone is brown to light gray, fine to medium grained, medium hard, fairly porous, tight, rarely. Although first described in the s, they are poorly known compared with Silurian elsewhere in Illinois. Recent sequence stratigraphic study of new subsurface samples, plus biostratigraphic and chemostratigraphic data, has clarified the nature of these rocks. The Silurian is divided into three unconformity-bound depositional sequences.


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A stratigraphic section through the Silurian turbidite sequence (Peary Land Group) in northern Nyeboe Land, north Greenland. by Poul-Henrik Larsen and Jan C. Escher Download PDF EPUB FB2

Stratigraphic section through the Silurian turbidite sequence (Peary Land Group) in northern Nyeboe Land, North Greenland. Copenhagen: Grønlands geologiske undersøgelse, (OCoLC) Document Type: Book: All Authors / Contributors: Poul-Henrik Larsen; Jan C Escher; Grønlands geologiske undersøgelse.

The Aberystwyth Grits Group is a Silurian lithostratigraphic group (a sequence of rock strata) in mid name is derived from Aberystwyth in northern Ceredigion where the strata are well exposed in coastal cliffs. The Group comprises the Trefechan Formation and the underlying Mynydd Bach Formation.

The rocks of the Aberystwyth Grits Group have also previously been known as the Named for: Aberystwyth. The Upper Devonian turbidite sequence in the central and southern Appalachian basin reaches m in thickness and consists of siltstone turbidites interbedded.

both areally and vertically through the stratigraphic section. They indicate a uniform dispersal pattern, transverse to the basin axis, for nearly km along depositional strike. The Silurian, named after the Silures tribe of Wales, begins during the recovery from the two-phased mass extinction that accompanied the pair of major glacial and interglacial events of the early and middle part of the Hirnantian Stage of latest Ordovician.

The Global Boundary Stratotype Sections and Points (GSSPs) for the four Silurian series—Llandovery, Wenlock, Ludlow, and Pridoli. Sequence stratigraphy of the Miocene section, southern Gulf of Mexico A sequence stratigraphic framework was proposed based on genetic sequences.

This study focuses on the interpretation of stratigraphic sequences through the integration of biostratigraphic, well log and 3D seismic data.

Sequence analysis is used to identify significant Cited by: 7. Free Web tutorials sequence stratigraphy, tutorials carbonate petrology, seismic interpretation sequence stratigraphy exercises Lower Cretaceous South Africa, seismic interpretation sequence stratigraphy exercises Bahamas Miocene, seismic interpretation sequence stratigraphy exercises Lower Cretaceous Alaska, clastic outcrop interpretation sequence stratigraphy exercises of.

Schematic cross section through the east flank of the Cincinnati Arch from the Lexing- Stratigraphy of the Bedford-Berea sequence along the western outcrop of the. land Rim section contains local Silurian carbonates, Devonian and Mississippian black shales, called.

Silurian Slope Turbidites: A Predictive Sequence Stratigraphic Model for the Exploration for New Accumulations of Mid-Qusaiba Sand Reservoir, Saudi Arabia.

By Riyadh A. Rahmani 1 (1) Saudi Aramco, Dhahran, Saudi Arabia perhaps through reactivation of older basement faults. Enhancing Sequence Stratigraphic Concepts Through the Integration of Seismic Stratigraphy and Seismic Geomorphology with Process Sedimentology—Positive Feedback Loops that Result in Improved Stratigraphic and Lithologic Predictions Eustatic Driver and Stratigraphic Response in an Ancient Continent Margin Turbidite System, Neoproterozoic.

stratigraphy: Walther’s law of facies. SUCCESSIONS OF STRATA Now think about the sequence of strata you would see in one big outcrop, or in a series of outcrops in a small area. This is called a local section. Even though the physical dimensions of the outcrop might be fairly. The simplest way to record the details of a surface outcrop is by measuring and describing a vertical stratigraphic section.

Ideally, the location of the section should be chosen to include important stratigraphic features, such as formation contacts, but, in practice, the location is commonly determined by accessibility-the presence of bars or beaches allowing us to walk along a river cut or.

cided to investigate a deep-water section where rates ofdeposition and erosion are tion cho-sen was across the Ordovician-Silurian boundary exposed at Dob's Linn, Scotland (Fig.

This stratigraphic section includes N 60 40W 20 Fig. Index map showing Ordovician-Silurian outcrops along the English. The fine-grained “shale” deposits host a vast amount of unconventional oil and gas resources. This chapter examines the variations in lithofacies, patterns of well logs, geochemistry, and mineralogy in order to construct a sequence stratigraphic framework of the representative marine Barnett, Woodford, Marcellus, Mowry, and Niobrara fine-grained “shales” (USA) and the marine Longmaxi.

Sequence stratigraphical concepts are applied to a 55 km long transect through the uppermost Ordovician and lower Silurian rocks of the Welsh Basin and the adjoining Midland Platform.

In summary this section explains how “ sequence stratigraphy ” can be used to study sedimentary rock relationships within a time-stratigraphic framework of. Lyell’s premise in& that “the present is the key to the past” is fundamental to sequence stratigraphy's recognition that the sedimentary record of the earth’s crust is the product of uniform and common physical processes that interacted with sediments as they accumulated.

This means that the processes responsible for known portions of a geological section can be. Hampshire County, W. (section C-C′, fig. The stratigraphic framework of the Cambrian and Ordovician sequence along this cross section and, to a lesser extent, the structure of the underlying block-faulted basement rocks are the main topics of this paper.

Cross section C-C′ is the third in a series of restored stratigraphic cross. Stratigraphy of Permian Basin of West TXspecial references to cross sections, Special Publication: North-South Cross Section, Pre-Miss.

Lamb Co. to Sw Kinney Co. March, through El Paso: Full Color Cross Section: Spring Field trip to Chinati Mountains, Presidio Co. Texas, May, Guidebook: The opportunity to see the stratigraphic fill for the Tanqua subbasin from the deepwater fans, through the slope and shelf margin to shallow marine and fluvial systems.

The deepwater elements form the focus of the course itinerary. Approximate Itinerary. Day 0 Arrival in Cape Town. Day 1 Breakfast meeting including course and driver safety. Lower Paleozoic stratigraphic and biostratigraphic correlations in the Canadian Cordillera: implications for the tectonic evolution of the Laurentian margin and distal turbidite flows suggest the margin was characterized by intervals of volcanism, basin foundering, and platform flooding.

Hirnantian (Ordovician) through Wenlock (Silurian. Silurian and Devonian carbonates Ordovician and SJurian clastics Ordovician black shale Cambrian and Ordovician carbonates Cambrian clastics Fig.

2. Stratigraphic cross-section of the Appalachian Basin showing the cyclic relationship of the basin fill. The Devonian black shale is the basal sequence .section shows the stratigraphic framework, depositional set-ting, sequence stratigraphy, and hydrocarbon-producing inter-vals of the Lower Silurian sandstone reservoirs and adjoining strata.

Cross section F–F′ presented here is about mi long and trends .Stratigraphic model and dipmeter in scree slope environment. Sand Dunes There are three major types of dunes: transverse, barchan, and seif dunes.

Each has a distinctive cross section or cross-bedding pattern. Parabolic dunes are similar to a single lobe of a barchan dune.