2 edition of stratigraphy and structure of the Ketilidian rocks of Midternaes, South-West Greenland found in the catalog.
stratigraphy and structure of the Ketilidian rocks of Midternaes, South-West Greenland
A. K. Higgins
Bibliography: p. -96.
|Statement||by A. K. Higgins.|
|Series||Meddelelser om Grønland, bd. 189, nr. 2, Grønlands geologiske undersøgelse. Bulletin no. 87, Meddelelser om Grønland ;, bd. 189, nr. 2., Bulletin (Grønlands geologiske undersøgelse) ;, no. 87.|
|LC Classifications||Q115 .D39 bd. 189 nr. 2|
|The Physical Object|
|Number of Pages||96|
|LC Control Number||70593730|
Buy Tertiary stratigraphy and paleobotany of the Cook Inlet region, Alaska, , Geological Survey Professional Paper, PA. on FREE SHIPPING on qualified orders. A summary of Tertiary volcanic stratigraphy of the southwestern high plateaus and adjacent Great Basin, Utah [D H et al Richter] on *FREE* shipping on qualifying offers.
The geology and petrology of the Precambrian rocks to the north-east of the Fjord Qagssit, Frederikshåb district, south-west Greenland. Meddelelser om Grønland ; 98 pp., 23 fig., 7 photoplts., 4 fold. plts. w. maps in pocket. on age, stratigraphy, and plate reconstructions: Comment and Reply Figure 1. Devonian-Carboniferous stratigraphy of East old names of Bütler () preferred by Hartz et al. () for the Devo-nian basin are shown together with the modern stratigraphic scheme of Olsen and Larsen ().Uppermost Devonian–Carboniferous data are.
Lists of fossiliferous stratigraphic units in North America; References. Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Dependencies: Denmark, Greenland, France, Clipperton . ining Cambrian rocks in an area of complex geology covering more than 70 square miles. Most of the sec tions were rather hurriedly measured and described, and the thickness of some was only visually estimated. The rock-stratigraphic classification is thought to be a substantial refinement of Mertie's (, p. ) origCited by:
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4 STRUCTURAL ASPECTS OF KIMBERLITE DYKE AND SHEET INTRUSION IN SOUTH-WEST GREENLAND By JAMES R. ANDREWS* and C. EMELEUS| ABSTRACT Kimberlite intrusions at three localities have been mapped in detail.
Geol. Soc. Afr. 71, HIGGINS, A. () The stratigraphy and structure of Ketilidian rocks of Midternaes, South-west Cited by: Structural aspects of kimberlite dyke and sheet intrusion in south-west Greenland.
A.K. HigginsThe stratigraphy and structure of Ketilidian rocks of Midternaes, South-west Greenland. Bull. Grønlands Geol. Unders, 87 () Also. Google Scholar. A.K. HigginsThe stratigraphy and structure of Ketilidian rocks of Midternaes, South-west Cited by: Graenseland and Midternaes are located in the northwestern Border Zone of the Paleoproterozoic Ketilidian orogen (Garde et al.
), between the Archean cratonic foreland to the north, and the. New evidence for a large Palaeoproterozoic impact: Spherules in a dolomite layer in the Ketilidian orogen, South Greenland The stratigraphy and structure of the Ketilidian rocks of Midternæs.
Stratigraphy, structure and petroleum potential of the Lady Franklin and Maniitsoq Basins, offshore southern West Greenland Article in Petroleum Stratigraphy and structure of the Ketilidian rocks of Midternaes 12(3) August with 30 Reads.
Greenland is the largest island in the northern hemisphere with a length of coastline bordering the Atlantic of G. and Pulvertaft, T. R.,The stratigraphy and structure of the Precambrian rocks of the and their relationships with Ketilidian supracrustals in the Ivigtut region, South-West Greenland: Rapp.
Grønlands Cited by: Analysen orogener und kratonischer Strukturen aus der Tiefenzone. The stratigraphy and structure of the Ketilidian Rocks of Midternaes, South-West Greenland.
- Bull. Grö nlands geol. Unders., Nr. 87, 1–96, A. Analysen orogener und kratonischer Strukturen aus der Tiefenzone. Geol Rund 34–44 (). https Cited by: 2. The north-west alignment of the Quantock Hills is controlled by the Cothelstone Fault (at present largely mantled by New Red Sandstone), having approximately three miles of dextral horizontal displacement and feet of vertical downthrow to the south-west.
A narrow zone of crumpled slates is developed adjacent to this fault near by: The present-day structure of the North Atlantic Ocean is dominated by the mid-Atlantic ridge and the three major crustal plates which meet at (and probably originate at) this feature.
These major Cited by: 5. 8 LAUGE KOCH: Stratigraphy of Northwest Greenland. contents of orthorhombic pyroxene (broncite or hypersthene)«. Low 22c mentions granite (see particulars below). The stretch of coast between Etah and the Humboldt Glacier has been described by KANE»This northern face of Greenland is broken by two large bays, at the base ofFile Size: 7MB.
Add tags for "The stratigraphy and structure of the Ketilidian rocks of Midternaes, South-West Greenland,". Be the first. Nalunaq is an orogenic, high gold grade deposit situated on the Nanortalik Peninsula, South Greenland.
Mineralisation is hosted in shear zone-controlled quartz veins, located in fine- and medium-grained amphibolite. The deposit was the site of Greenland’s only operating metalliferous mine until its closure inhaving produced t of gold. This study uses a combination of field Cited by: 5. In Midternaes and northern Graenseland the supracrustal rocks rest unconformably on the Archaean basement and are metamorphosed only at sub-greenschist grade, but.
Stratigraphy of the Keku Islets and Neighboring Parts of Kuiu and Kupreanof Islands Southeastern Alaska [MUFFLER (L.J. Patrick)] on *FREE* shipping on qualifying offers. Stratigraphy of the Keku Islets and Neighboring Parts of Kuiu and Kupreanof Islands Southeastern AlaskaAuthor: MUFFLER (L.J.
Patrick). ELSEVIER Precambrian Research 86 () 59 70 Prernmbriun Resenr(h Field recognition of rocks totally retrogressed from granulite facies: an example from Archaean rocks in the Paamiut region, South-West Greenland V.R.
McGregor a, C.R.L. Friend b a Atammik, DK Maniitsoq, Greenland, Denmark b Department of Geology, Oxford Brookes University, Oxford, OX30BP, UK Received 16 Cited by: During Renzy Mines Ltd. exploration programme inan iron-formation was found in the Midternæs area north east of Ivigtut, South-West Greenland.
It contains up to % Fe. The dominant mineral is greenalite, with minor amounts of magnetite, siderite and quartz. It was found in the northernmost part of the Ketilidian supracrustals (. m.y.), which are non-metamorphosed or Cited by: 4.
They were accreted in juvenile calc-alkaline arcs at ca. – Ma (Kalsbeek et al., ), and they are in many respects similar to the somewhat younger (and better preserved) rock units in the Ketilidian orogenic belt of South Greenland (Garde et al., ).
Prior to the Caledonian orogeny, these Precambrian basement complexes within the. Mapping at scale on the central Graham Island has shown that Cretaceous strata are more widely distributed than previously known.
This study examines the stratigraphy and structural geology of the Cretaceous rock sequence, and also addresses the petroleum potential of these units. At the base is the Cretaceous sandstone unit.
This unit is divided into three lithofacies. The massive. The Paleoproterozoic orogens in Greenland, from north to south, are the Inglefield mobile belt ( Ga), the Rinkian fold belt/Nagssugtoqidian orogen ( Ga) and the Ketilidian orogen. Prior to the tectono-stratigraphic terrane model, field geologists sought to reconcile the field interpretations and isotopic data by suggesting that granulite facies metamorphism could flush-out the radiogenic Sr and Nd accumulated in rocks since the early Archaean to ‘reset’ the whole rock ages (Collerson et al., ).Cited by: 6.
Abstract: Lower Cretaceous Stratigraphy and Source Rock Distribution in Pre-salt Basins of the South Atlantic: Comparison of Angola and Southern Brazil. Pasley, Mark A. and Edith Newton Wilson - Amoco; Vitor S. Abreu - Rice University; Mário G.
P. Brandão - Sonangol; and Augusto Silva Telles - .Buy Geology of the Golconda Quadrangle: A Detailed Report on the Stratigraphy and Structure of That Portion of the Golconda Quadrangle Lying in Kentucky (Classic Reprint) on FREE SHIPPING on qualified orders.overlying the Archean granite basement rock of the Kaapvaal craton.
The country rocks around the Uitkomst Complex are discussed in more detail in Chapter 2. The Uitkomst Complex has been suggested to be genetically related to the Ma, Bushveld Igneous Complex (BIC; de Waal and Gauert, ), also hosted within the Kaapvaal craton by.