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1 edition of Tectonic Assemblages of Ontario, 1993-Data Set 11 [CD-ROM] found in the catalog.

Tectonic Assemblages of Ontario, 1993-Data Set 11 [CD-ROM]

Tectonic Assemblages of Ontario, 1993-Data Set 11 [CD-ROM]

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Published in Sudbury :MNDM, 1993 .
Written in English


ID Numbers
Open LibraryOL19820514M

Urban geoscientific data of East and Southeast Asia: GIS data sets of 11 cities This CD-ROM set is the final product of the DCGM III Project. It is a feasibility study of the application of geological data for preliminary urban planning.   consists of autochthonous assemblages of 2, to 2,million-year-old metavolcanic rocks and their intrusive equivalents, which are unconformably or disconformably overlain by the Ma Porcupine and 2, to 2,million-year-old Timiskaming metasedimentary assemblages .

A CD-ROM of datasets and computer coding using programs such as WinBUGS and S-PLUS accompanies the book. Catalog no. , ISBN: March , 7 x 10, pp. Suggested Price: $ The Independence Creek (“Boulevard”) area in the Dawson Range district in west-central Yukon has recently received new government geological mapping; however, little is known about the nature or origin of gold mineralization in this region. A regional metallogenic framework for the mineralization is proposed herein, based on geological, structural, geochronological, and fluid inclusion.

  Adams, P.M., and Anderson, J.L., , Occurrence of clintonite-monticellite-idocrase assemblages in contact skarns of the Clark Mountain thrust complex, NE San Bernardino County, California: Geological Society of America, Abstracts with Programs, v. L.D. and Ray, G.E., b, Tectonic Controls on Precious Metal Enriched Skarn. Bull, William B. Tectonic Geomorphology of Mountains 11 Bul Blackwell Publishing Bull, William B. Tectonic Geomorphology of the Mountains 11 12 Bul Blackwell Publishing Bullard, Fred M. The Story of El Paricutin. B-1 7 The Scientific Monthly, vol. LXV, no.5, Nov.


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Tectonic Assemblages of Ontario, 1993-Data Set 11 [CD-ROM] Download PDF EPUB FB2

2. Tectonic and geophysical background. The Canadian Shield, the Precambrian core of North America, is an assemblage of tectonic provinces with very different ages and histories (Hoffman, ).One of these provinces is the Proterozoic Grenville Province, forming a belt ≈ – km wide along the southeastern margin of the Canadian Shield (Fig.

1, inset).Cited by: 2. Based on geochronological information, six volcanic assemblages are distinguished that formed by submarine volcanic activity between ca.

and Ma. These assemblages are referred to, from oldest to youngest, as the Pacaud, Deloro, Stoughton-Roquemaure, Kidd-Munro, Tisdale, and Blake River assemblages. The polyphase evolution of the Seridó Belt (NE-Brazil) includes D 1 crust formation at – Ga, D 2 thrust tectonics at Ga and crustal reworking by D 3 strike-slip shear zones at Ma.

Microstructural investigations within mylonites associated with D 2 and D 3 events were used to constrain the tectono-thermal evolution of the belt.

D 2 shear zones commenced at deeper crustal levels Cited by:   Uncertainty into the nature and presence of pre-plate tectonic regimes and the timing of any change in tectonic regimes relates to the incompleteness of the rock archive in deep time, differences in the criteria used to infer the existence of plate tectonic and pre-plate tectonic regimes on the early Earth (ca greater than Ga), and Cited by: Tectonic map of North America, showing location of the Archean Superior Province at the core of the Canadian Shield (after Hoffman, ).

Unlabelled white areas are knowledge gaps due to lack of. Schematic diagram illustrating methodology of combined regional and metallogenic and tectonic analysis of cratons, terranes, accretionary assemblages, post-accretopmaru overlap assemblages, and.

[6] A set of northwest trending regional isograds parallel the structural grain of the region except where they are at a high Tectonic Assemblages of Ontario to the traces of F 2 structures south of the Bigmouth pluton (Figures 4 and 5).

The lowest‐grade, chlorite‐bearing assemblages are located in the west flank of the fan in the immediate hanging wall of the. A set of sheeted quartz veins cutting Ma monzogranite at Sandwich Point, Nova Scotia, Canada, provide an opportunity to address issues regarding fluid reservoirs and genesis of intrusion-related gold deposits.

The quartz veins, locally with arsenopyrite (≤5%) and elevated Au–(Bi–Sb–Cu–Zn), occur within the reduced South Mountain Batholith, which also has other zones of anomalous. texts All Books All Texts latest This Just In Smithsonian Libraries FEDLINK (US) Genealogy Lincoln Collection.

Understanding 9/ Software Sites Tucows Software Library Shareware CD-ROMs Software Capsules Compilation CD-ROM Images ZX Spectrum DOOM Level CD.

Understanding 9/ Spirituality & Religion Sports Videos Television Videogame Videos Vlogs Youth Media. Audio Books & Poetry Community Audio Computers, Technology and Science Music, Arts & Culture News & Public Affairs Non-English Audio Spirituality & Religion.

Librivox Free Audiobook. During Jurassic and Early Cretaceous time, arc magmatism in the Klamath Mountains province was episodically punctuated by contractional deformation (Wright and Fahan, ; Hacker and Ernst, ; Hacker et al., ).These contractional events are represented by regional thrust faults that separate distinct, commonly arc-related, tectonostratigraphic terranes (Irwin,Access: CD-ROM [] or CD-ROM [] Description: The Tectonic Geology Data Set is a digital interpretation of the Tectonic Geology of the Province of Ontario, It illustrates this by 1) grouping volcanic and sedimentary rock units into tectonic assemblages in Precambrain terrains and depositional sequences in the overlying Paleozoic and.

The assemblages define a metamorphic field gradient (see Chap. 3) and rocks on this P–T-array are said to be of low grade at low P–T and of successively higher grade with higher P–T conditions.

The term metamorphic grade is a qualitative indicator of the physical conditions that have been operating on the rocks. 11 ORBITAL FORCING Introduction The nature of Milankovitch processes Components of orbital forcing Basic climatology Variations with time in orbital periodicities Isostasy and geoid changes Nonglacial Milankovitch cyclicity The nature of the cyclostratigraphic data base The geologic.

A detailed study of the geochemical and isotopic characteristics of the volcanic rocks of the Hidden and Louis formations, which make up the hanging wall to the volcanogenic massive sulphide deposi.

For the Second Edition of Earth Structure: An Introduction to Structural Geology and Tectonics, the authors have heavily revised each chapter while preserving the overall structure of the First Second Edition also benefits from new artwork that clearly illustrates complex concepts.

GIS Data at the University of Toronto Map Library. Please read the Conditions of Use for Electronic Resources web page for more information on the restrictions on. The following set of three arrivals has five ray legs in the soft layer (two bounces); the next set has seven legs (three bounces).

Blue letters below the trace denote the time interval between arrivals, which is either the two‐way P travel time (2P) or the time difference between an S and a P leg in the soft layer.

2. Geologic framework. In common with other Early Archaean rocks of the outer Godthåbsfjord region (figure 1), two main lithologic assemblages comprise rocks on Akilia and most abundant is approximately – Gyr composite, banded, tonalitic gneisses (Nutman et al.; Whitehouse et al.

), historically referred to as the Amîtsoq gneisses. Abstract U/Pb zircon/titanite geochronology, in situ monazite geochronology, and 40Ar/39Ar thermochronology provide an unusually complete data set for reconstructing the tectonic history of Proterozoic rocks exposed in the Black Canyon, Gunnison, Colorado.

These new geochronologic data record three protracted orogenic episodes and an exhumation event between orogenic pulses: (1). The compositional Se has been quantitatively determined with TCF-INAA in the NIST variability increases still further in the mineralized assemblages of Stage III, in series of glass and a set of selenium-doped NiS beads have been produced with which sulphides exhibit the range + to +, chalcopyrite generally selenium concentration.Furthermore, the digitised geological maps (on the attached CD-ROM) are correlated and harmonised according to the current stratigraphic time table.

The atlas aims to contribute to capacity building in African Earth Sciences and to initiate research and economic opportunities by providing a database of basic geological background information.Volcanoes of the Antarctic Plate and Southern Ocean (Vol.

48). American Geophysical Union, LeMasurier, W. E., & Rex, D. C. (). Volcanic record of Cenozoic glacial history in Marie Byrd Land and western Ellsworth Land: Revised chronology and evaluation of tectonic factors. Antarctic Geoscience, 89,