Crustal Evolution and Composition Beneath Southern Africa
Author | : Shaji Nair |
Publisher | : |
Total Pages | : 126 |
Release | : 2005 |
Genre | : |
ISBN | : |
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Author | : Shaji Nair |
Publisher | : |
Total Pages | : 126 |
Release | : 2005 |
Genre | : |
ISBN | : |
Author | : A. J. Tankard |
Publisher | : Springer Science & Business Media |
Total Pages | : 528 |
Release | : 2012-12-06 |
Genre | : Science |
ISBN | : 1461381479 |
Syntheses of the geology of major areas of the Earth's crust are increasingly needed in order that the features of, and the problems associated with, the secular evolution of the continents can be understood by a wide audience. Southern Africa is fortunate in having a remarkable variety of geological environments developed without many breaks over 3. 8 Ga, and many of the rock groups are household names throughout the geological world. In one respect the geology of Southern Africa is particularly important: cratonization clearly began as early as 3. 0 Ga ago, in contrast to about 2. 5 Ga in most other continental areas such as North America. This book documents very well the remarkable change in tectonic conditions that took place between the Early and Mid-Precambrian; we have here evidence of the very earliest development of rigid lithospheric plates. This book is a tribute to the multitudes of scientists who have worked out the geology of Southern Africa over many years and decades. Whatever their discipline, each provided a step in the construction of this fascinating story of 3. 8 Ga of crustal development. In the book the reader will find a detailed review of the factual data, together with a balanced account of interpretative models without the indulgence of undue speculation. One of its attractions is its multidisciplinary approach which provides a stimulating challenge to the reader.
Author | : Åsa Pettersson |
Publisher | : |
Total Pages | : 28 |
Release | : 2008 |
Genre | : |
ISBN | : |
Author | : Douwe J. J. van Hinsbergen |
Publisher | : Geological Society of London |
Total Pages | : 392 |
Release | : 2011 |
Genre | : Africa |
ISBN | : 9781862393356 |
The African continent preserves a long geological record that covers almost 75% of Earth's history. The Pan-African orogeny (c. 600-500 Ma) brought together old continental kernels (West Africa, Congo, Kalahari and Tanzania) to form Gondwana and subsequently the supercontinent Pangaea by the late Palaeozoic. The break-up of Pangaea since the Jurassic and Cretaceous, primarily through opening of the Central Atlantic, Indian, and South Atlantic oceans, in combination with the complicated subduction history to the north, gradually shaped the African continent. This volume contains 18 contributions that discuss the geology of Africa from the Archaean to the present day.
Author | : Alexandra Sabattier |
Publisher | : |
Total Pages | : 0 |
Release | : 2023 |
Genre | : |
ISBN | : |
In this thesis, new estimates of crustal thickness and structure obtained from H-[kappa] stacking of P-wave receiver functions and the joint inversion of P-wave receiver functions and Rayleigh wave group velocities are presented for 63 seismic stations in Mozambique, Namibia, Uganda, and South Africa. These new estimates are used to characterize the nature of the crust beneath the Mozambique Coastal Plains (MCP) in central and southern Mozambique and, when combined with previous estimates of crustal thickness and structure in sub-Saharan Africa, to investigate if there are secular changes in crustal genesis through the Precambrian. Moho depths beneath 29 broadband seismic stations in Mozambique indicate crustal thicknesses between 23 and 43 km. Moho depths beneath nine stations in Uganda vary between 36 and 43 km. Crustal thickness beneath 19 stations in Namibia ranges from 35 and 48 km, and for six stations in South Africa between 33 and 43 km. The 1-D velocity models for all stations in Precambrian terranes yield an average Vs of 3.7 to 3.8 km/s and show some high velocity (Vs > 3.9 km/s) layers in the lower crust indicating the presence of mafic lithologies. New results reported in this thesis, when combined with results from previous studies in sub-Saharan Africa, yield an average crustal thickness for all Precambrian terranes of 39 ± 4 km. The average crustal thicknesses are found to be almost identical for Archean (39 ± 2 km) and Proterozoic (39 ± 3 km) terranes. The average crustal thicknesses for terranes of all eras fall between 38 and 40 km. Furthermore, the average thickness of the mafic lower crust is almost identical in Archean and Proterozoic terranes (7 ± 4 km and 6 ± 4 km, respectively). In addition, the average crustal shear wave velocities for all terranes fall within one standard deviation of the overall mean velocity of 3.7 km/s. These results are consistent with findings in previous studies highlighting a lack of evidence for secular variation in the crustal structure or composition within Precambrian terranes in eastern and southern Africa, suggesting that secular changes, if they existed, have been obscured by tectonic reworking of crustal structure and composition by later orogenic and/or magmatic events. New results from 14 seismic stations in the MCP reveal sediment thicknesses ranging from 3 to 9 km and Moho depths ranging from 23 to 32 km. An average crustal Vs of 3.6 to 3.7 km/s, together with the lack of high velocity (i.e., Vs > 3.9 km/s) layers in the crust, suggests the crust is stretched continental crust and not oceanic crust.
Author | : K.C. Condie |
Publisher | : Elsevier |
Total Pages | : 553 |
Release | : 1993-02-03 |
Genre | : Science |
ISBN | : 0080869092 |
As a final product of the International Geological Correlation Program (IGCP) Project 217, this volume brings together significant advances in the understanding of Proterozoic crustal evolution. This IGCP Project focussed on nine research objectives: 1) Comparison of Archean and Proterozoic supracrustal assemblages to more fully understand differences between Archean and post-Archean tectonic regimes; 2) To more fully understand the geochemical differences between Archean and post-Archean sediments and to evaluate the various factors that control sediment composition; 3) From combined U/Pb zircon and whole-rock Sm/Nd studies, to see if the apparent 2.4-2.0 continental crust "generation gap" is real; 4) To employ new techniques in the dating of individual zircons to more fully understand Proterozoic tectonic history and the role of crustal reworking; 5) From trace element ratios and Nd isotopic data from basalts, to better understand Proterozoic mantle evolution; 6) To encourage more detailed studies of the anorogenic granite-anorthosite association to better understand its origin and significance in terms of crustal evolution; 7) From combined Nd, Pb, and Sr isotopic data, to more precisely estimate the amount of new continental crust formed during the Proterozoic; 8) To encourage joint P-T and geochronological studies of Proterozoic and high-grade terranes to better understand Proterozoic orogenesis: and 9) To try and understand why hydrothermal precious metal deposits are relatively rare in the Proterozoic compared to both the Archean and the Phanerozoic. The book should be of interest to professionals in the geosciences (especially geochemists, petrologists and structural geologists) and graduate students in the same fields.
Author | : Barbara Romanowicz |
Publisher | : Elsevier |
Total Pages | : 873 |
Release | : 2010-04-20 |
Genre | : Science |
ISBN | : 0444535756 |
Treatise on Geophysics: Seismology and Structure of the Earth, Volume 1, provides a comprehensive review of the state of knowledge on the Earths structure and earthquakes. It addresses various aspects of structural seismology and its applications to other fields of Earth sciences. The book is organized into four parts. The first part principally covers theoretical developments and seismic data analysis techniques from the end of the nineteenth century until the present, with the main emphasis on the development of instrumentation and its deployment. The second part reviews the status of knowledge on the structure of the Earths shallow layers, starting with a global review of the Earth's crustal structure. The third part focuses on the Earth's deep structure, divided into its main units: the upper mantle, the transition zone and upper-mantle discontinuities, the D region at the base of the mantle, and the Earth's core. The fourth part comprises two chapters which discuss constraints on Earth structure from fields other than seismology: mineral physics and geodynamics. Self-contained volume starts with an overview of the subject then explores each topic with in depth detail Extensive reference lists and cross references with other volumes to facilitate further research Full-color figures and tables support the text and aid in understanding Content suited for both the expert and non-expert
Author | : Heinrich D Holland |
Publisher | : Academic Press |
Total Pages | : 681 |
Release | : 2010-05-25 |
Genre | : Science |
ISBN | : 0123813921 |
Readings from the Treatise on Geochemistry offers an interdisciplinary reference for scientists, researchers and upper undergraduate and graduate level geochemistry students that is more affordable than the full Treatise. For professionals, this volume will provide an overview of the field as a whole. For students, it will provide more in-depth introductory content than is found in broad-based geochemistry textbooks. Articles were selected from chapters across all volumes of the full Treatise, and include: The Origin and Earliest History of the Earth, Compositional Evolution of the Mantle, Evolution of Sedimentary Rocks, Soil Formation, Geochemistry of Groundwater, Geologic History of Seawater, Hydrothermal Processes, and Biogeochemistry of Primary Production in the Sea. Comprehensive, interdisciplinary and authoritative content selected by leading subject experts Robust illustrations, figures and tables Affordably priced sampling of content from the full Treatise on Geochemistry
Author | : Preston Cloud |
Publisher | : |
Total Pages | : 40 |
Release | : 1976 |
Genre | : Earth |
ISBN | : |
Author | : Louis Charles Pakiser |
Publisher | : Geological Society of America |
Total Pages | : 843 |
Release | : 1989 |
Genre | : Science |
ISBN | : 081371172X |
A review and evaluation of our knowledge of the structure of the crust and upper mantle of the continental United States, exclusive of Alaska, as determined from geophysical observations. Covers geophysical methods of studying the crust and upper mantle; a region-by-region review of crustal and upper-mantle structure; continental overviews based on the different geophysical methods; and geologic and petrologic syntheses based largely on the geophysical results.