ALBERT

Description / Table of Contents: INTRODUCTION The study is essentially empirical, since it portrays and appraises two different water management systems, and relates them to one another. Yet the analysis has also been made with definite research aims in mind. Its focus has been narrowed down to the environmental assessment of urban water management systems in arid and semi-arid regions, especially with an eye to deal with information problems in the Developing World. The study addresses a set of very critical issues of global concern, and, thus, delineates a crucial topic for international research. The fact that a wide range of critical issues usually complicates and aggravates the given problem setting provides the comparative analysis with a special practical incentive to explore the opportunities for joint strategies and comprehensive solutions. However, the complexities involved between water management and the environment and the relative lack of a joint theory in that field pose certain difficulties to such an undertaking. In order to fully appreciate the underlying purpose of the study and the scope of its implications, the various facets of the problem setting and the essential ingredients of the general line of approach have first to be unravelled and expounded at some length. Above all, it needs to be shown how these facets combine to produce the complex, burning issues which in turn seem to, both in theory and practice, require correspondingly intricate, strategic approaches for their solutions...

Description / Table of Contents: PREFACE The emergence of new information from drilling in deep-sea and coastal areas and the surfacing of the plate tectonics theory probably had the greatest impacts in recent decades on the highly accelerated growth of knowledge regarding the evolution of sediments and sedimentary rocks. Studies in recent years have also provided new insights on global sedimentary processes, and isotopic tools in many ways have enhanced our knowledge and have provided even an unexpected added dimension to the mechanisms of some specific processes. Many different uses of isotopic tools in studies of sedimentary processes can be found in the literature, but the information is highly scattered in the vast field of sedimentology. The disseminated state of existing isotopic knowledge on sedimentary systems has undoubtedly deprived many practitioners in the field to fully appreciate the benefits and limitations, and even the apparent confusion, concerning the use of isotopic tools. We have endeavored here to bring together discussions on some major sedimentary systems in the sedimentary cycle and to analyze them according to isotopic evidence. To accomplish such a task required contributions from many individuals. We were fortunate to have friends who accepted to share our goals. We most sincerely thank all the contributors to this book and deeply appreciate their patience and fortitude despite our undue demands on them to reach our objectives...

Description / Table of Contents: Introduction / Pages 1-32 --- Interpretation using nomograms / Pages 33-47 --- Linear parameters / Pages 49-114 --- Non-linear parameters / Pages 115-173 --- Maximum likelihood and maximum entropy / Pages 175-193 --- Analytic inversion / Pages 195-211 --- Advanced inversion methods / Pages 213-227 --- Error analysis / Pages 229-243 --- Parallel computation in modelling and inversion / Pages 245-255

Description / Table of Contents: PREFACE This book represents the first attempt in three decades to marshall out available information on the regional geology of Africa for advanced undergraduates and beginning graduate students. Geologic education in African universities is severely hampered by the lack of a textbook on African regional geology. This situation is greatly exacerbated by the inability of most African universities to purchase reference books and maintain journal subscriptions. Besides, geologic information about Africa is so widely dispersed that a balanced and comprehensive course content on Africa is beyond the routine preparation of lecture notes by university teachers. Since geology is a universal subject and Africa is one of the largest landmasses on Earth with one of the longest continuous records of Earth history, there is no doubt that geologic education in other parts of the world will benefit from a comprehensive presentation of African geologic case histories. The scope of this text also addresses the need of the professional geologist, who may require some general or background information about an unfamiliar African geologic region or age interval. Africa occupies a central position in the world's mineral raw materials trade. Because of its enormous extent and great geologic age, the diversity and size of Africa's mineral endowment is unparalleled. Africa is the leading source of gold, diamond, uranium, and dominates the world's supply of strategic minerals such as chromium, manganese, cobalt, and platinum. Consequently, African nations from Algeria to Zimbabwe depend solely on mineral exports for economic survival. The geologic factors which govern economic mineral deposits are stressed in this text. The geological history of Africa spans 3.8 billion years, a record that is unique both in duration and continuity. Few other parts of our planet match the plethora of geologic phenomena and processes that are displayed in the African continent. From the various stages of crustal evolution decipherable from the Archean of southern Africa, through the plate tectonics scenarios in the ubiquitous Late Proterozoic-Early Paleozoic Pan-African mobile belts and in the Hercynian and Alpine orogenies of northwest Africa, to the East African Rift Valley, Africa is replete with excellent examples and problems for a course on regional tectonics. Teachers of igneous and metamorphic petrology can hardly ignore Africa's anorogenic magmatism (e.g.. layered ultramafic intrusives such as the Great Dyke and the Bushveld Complex; the Tete gabbro-anorthosite pluton; alkaline complexes; basaltic volcanism), or tantalizing highgrade metamorphic terranes such as the Limpopo belt, the Namaqua mobile belt, and the Mozambique belt. From the extensive Precambrian supracrustal sequences throughout the continent with enormous thicknesses of sedimentary rocks that have hardly been deformed or metamorphosed, to the stratigraphic evolution of Africa's present-day passive continental margin, there is a complete spectrum of facies models upon which to base a course on basin analysis and stratigraphy. To maintain its integrity a course on historical geology anywhere in the world must address the theory of Continental Drift beyond invoking past continuities between West Africa and South America. Past connections between West Africa and eastern North America must equally be explored, so also connections between northeast Africa and Arabia, and the paleogeography of southern Gondwana where Africa occupied centre stage. The Precambrian fossil record, the transitions from reptiles to the earliest mammals and dinosaurs, and the evolution of Man are among Africa's unique contributions to the history of life and the story of organic evolution. Although it lies today in the tropics Africa was the theatre of the Earth's most-spectacular glaciations. Even after the scene of continental glaciation had shifted to the northern continents only lately during the Pleistocene, Africa still witnessed spectacular climatic fluctuations during the Quaternary. Certainly students of archeology and paleoanthropology cannot overlook the Quaternary paleoenvironmental record of the Olduvai Gorge in Tanzania, the Lake Turkana basin in Kenya, the Nile valley, the Sahara, and southern Africa. But since African examples have already been cited in standard geologic textbook, I have often been asked why it has become necessary to revive the idea of a full-length textbook on African geology, 30 years after this idea was abandoned by the geologic community. My simple answer, as already stated, is that the wealth of available geologic information about Africa is so enormous and fascinating, but so diffuse, that an attempt must be made to assemble and pass on this knowledge.

Description / Table of Contents: INTRODUCTION The International Summer School of Theoretical Geodesy on Satellite Altimetry in Geodesy and Oceanography was held in Trieste (Italy) from May 25 to June 6, igg2. It was organized by Prof. R. Rummel of the Delft University of Technology and by Prof. F. Sansò of the Politecnico di Milano and was attended by 63 participants and 7 lecturers from 17 countries. The School was hosted by the International Centre of Theoretical Physics of Trieste. Satellite altimetry provides a lot of data that require more and more sophisticated models in order to be interpreted and exploited. One of the main problems related to the practical treatment of the data can be summarized as follows: oceanographers would like to ask geodesists to compute precise orbits and a precise geoid in order to put into evidence the Sea Surface Topography that can be interpreted as an oceanographic signal related to currents and to several physical parameters; on the other hand, geodesists would like to ask oceanographers to a-priori determine the Sea Surface Topography, in order to be able to extract from the altimeter data the geoid and the orbit errors to be used in the gravity field modelling. The solution to this dilemma can only be found in a cooperative frame. An integrated model to be used for a single-step treatment of altimetry is probably far to be defined, so at present geodesists and oceanographers must cooperate to obtain step-wise and iterative modelling of the gravity field and of the oceanographic phenomena. This is precisely the reason why the school on Satellite Altimetry was organized on an interdisciplinary basis...

Description / Table of Contents: PREFACE Sedimentation as a Three-Component System describes the most common styles of deposition in marine environments as they relate to sediment composition. Three components, organic matter, carbonate, and siliciclastic sediment, may settle concurrently, but at different rates, intermixing on the sea floor to form a particular sediment composition. A change in the flux of one component is capable of relatively diluting or concentrating the other two components, which can be expressed in the characteristic ratio of organic carbon to carbonate in the resulting sediment. The basic concept of this book is to address organic carbon-carbonate associations in terms of depositional inputs and time spans. In addition, the three-component system describes organic carbon changes related to major facies transitions. Examples include models of the genesis of carbonaceous sediments, with their various laminated to bioturbated lithotypes, and numerical organic carbon prediction. I hope that this book will encourage stimulating discussions and promote a new approach to quantitative stratigraphy...

Description / Table of Contents: Chapter 1. High Resolution and Better Imaging --- MUSES-B Satellite System for VSOP / H. Hirosawa / pp. 3-9 --- Mechanical Design and Development of a Deployable Space Antenna for Japanese VLBI Space Observatory Program / M. C. Natori, T. Takano, K. Miyoshi, T. Inoue and T. Kitamura / pp. 10-20 --- Operation of the VSOP Satellite / Y. Murata / pp. 21-25 --- Ground Supporting Facilities for VSOP Observations / N. Kawaguchi, H. Kobayashi, T. Miyaji, H. Mikoshiba, A. Tojo, Z. Yamamoto and H. Hirosawa, / pp. 26-33 --- Space VLBI Simulations / D. W. Murphy, V. Yakimov, H. Kobayashi, A. R. Taylor and I. Fejes / pp. 34-38 --- Space VLBI Scheduling Studies: Techniques and Results / D. L. Meier / pp. 39-43 --- An Affordable Advanced Space VLBI Mission / J. S. Ulvestad, D. L. Meier, D. W. Murphy, R. A. Preston and J. G. Smith / pp. 44-48 --- Space VLBI Experiments Using ETS-VI / T. lwata, H. Kiuchi, M. Imae, M. Sekido and S. Hama / pp. 49-53 --- Space VLBI Polarization Observations / D. C. Gabuzda and A. R. Taylor / pp. 54-58 --- Space VLBI User Assistance Software / I. Fejes, D. W. Murphy, A. R. Taylor, V. Yakimov and G. Young / pp. 59-69 --- mm VLBI / L. B. Bååth / pp. 70-74 --- "High Sensitivity" VLBI at 86 GHz: First Fringes with the 100 m Radio Telescope at Effelsberg / K. J. Standke, D. A. Graham, T. P. Krichbaum, A. Witzel, C. J. Schalinski, A. E. E. Rogers, R. Booth, L. B. Bååth / pp. 75-85 --- Burst Mode System toward mJy Level mm-VLBI / M. Inoue, K. Matsumoto and N. Kawaguchi / pp. 86-88 --- 86 GHz Global VLBI Progress Report / S. Doeleman, A. E. E. Rogers, L. Bååth, C. Schalinski, T. Krichbaum, M. Inoue, A. Zensus, S. Padin, J. Carlstrom, D. Graham, C. Predmore, J. Moran, D. Backer, M. Wright, N. Whyborn, L. Nyman, K. Standke, M. Lerner and S. Kameno / pp. 89-92 --- Global 3- and 7-mm VLBI Observations of OJ287 / C. E. Tateyama and M. Inoue / pp. 93-100 --- VLBI Observations of the 22 GHz H2 0Maser in Late Type Stars / H. Takaba, T. lwata, M. Miyoshi, N. Ukita, S. Kameno and K. Matsumoto / pp. 101-104 --- The H2 0 Super Maser Outburst Region in the Orion Nebula / L. I. Matveyenko and P. J. Diamond / pp. 105-109 --- The Cosmological Application of the VLBI Technique at Ultimate Resolutions / L. I. Gurvits / pp. 110-114 --- First VLBI Images of Supernova 1993J in the Galaxy M81 / N. Bartel, M. F. Bietenholz, M. P. Rupen, J. E. Conway, A. J. Beasley, R. A. Sramek, J. D. Romney, M. A. Titus, D. A. Graham, V. I. Altunin, D. L. Jones, A. Rius, T. Venturi, G. Umana, R. L. Francis, M. L. McCall, M. G. Richer, C. C. Stevenson, K. W. Weiler, S. D. Van Dyk, N. Panagia, W. H. Cannon, J. Popelar and R. J. Davis / pp. 115-122 --- The Visibility-Spectrum Relation among Radio Loud AGNs / S. Kameno, M. Inoue, K. Matsumoto, H. Takaba, T. lwata, R. Nan and R. T. Schilizzi / pp. 123-129 --- Identification of the Superluminal Motion in Faint Parsec-Scale Jet of 3C390.3 / S. Wu, E. Preuss, W. Alef, K. I. Kellermann and Y. Qiu / pp. 130-136 --- A VLBI Search for Compact Nonthermal Emission from the Herbig Be Star MWC 297 / S. L. Skinner and R. B. Phillips / pp. 137-140 --- Snapshot VLBI Mapping of Variable Extragalactic Sources at 327 MHz / L. I. Gurvits, W. Alef, D. R. Altschuler, J. E. Carson, B. Dennison, D. Graham and A. S. Trotter / pp. 141-145 --- AO 0235+164151;A "Heretic" BL Lac / H. S. Chu, L. B. Bååth, F. T. Rantakyrö, R. S. Booth, R. E. Spencer and F. J. Zhang / pp. 146-155 --- Chapter 2. Antenna and Networks --- The New Receiver in the S, X, K Bands for the VLB1 Medicina Dish / A. Orfei, G. Maccaferri, S. Mariotti, M. Morsiani, G. P. Zacchiroli and G. Tomassetti / pp. 159-164 --- The Upgrade Proposal for the VLBI Medicina Antenna / A. Orfei, G. Maccaferri, S. Mariotti, M. Morsiani and G. P. Zacchiroli / pp. 165-170 --- VLBI at the Kyushu Tokai University / M. Fujishita, K. Miyasato, T. Yoshiyama and Y. Matsumae / pp. 171-175 --- VLBI Activities at the Matera Space Geodesy Center / R. Lanotte, G. Bianco, M. Fermi and L. Garramone / pp. 176-184 --- The Mizusawa 10-m Antenna and Its VLBI Observation System / K. M. Shibata, Y. Asaki, I. Asari, Y. Fukuzaki, T. Hara, K. Horiai, K. lwadate, 0. Kameya, N. Kawano, S. Kuji, S. Manabe, S. Sakai, T. Sasao, K. Sato, Y. Tamura and S. Tsuruta / pp. 185-190 --- The 6 m VLBI Telescope at Kagoshima, Japan / T. Omodaka, M. Morimoto, N. Kawaguchi, T. Miyaji, S. Yasuda, T. Suzuyama, T. Kitagawa, T. Miyazaki, L. Furuya, T. Jike, K. Miyazawa, H. Mikoshiba, S. Kuji, 0. Kameya and Kagoshima VLBI Group / pp. 191-195 --- Radio Telescopes and VLBI Facilities in Brazil / P. Kaufmann and C. E. Tateyama / pp. 196-199 --- Cryogenic Cooled Receivers for the QUASAR Network / A. V. lpatov, I. A. lpatova and V. V. Mardyshkin / pp. 200-204 --- The Australian Long Baseline Array—Status Report / A. Tzioumis, W. Wilson and R. Ferris / pp. 205-210 --- The Asia-Pacific Telescope—APT / A. Tzioumis / pp. 211-217 --- Present Status and Future Development on VLBI Facilities in China / Ye S. and Oian Z. / pp. 218-220 --- Chapter 3. The New Trends in Geodesy and Astrometry --- Plate Dynamics near Boundaries: What Governs the Transition between Episodic and Continuous Motions? / K. Heki / pp. 223-228 --- Improved Global Atmospheric Mapping Functions for VLBI and GPS / A. Niell / pp. 229-231 --- Method of Differential Fringe Phase Tracking / N. Kawano, T. Sasao, T. Hara, S. Kuji, 0. Kameya, K. Sato, K. lwadate and Y. Asaki / pp. 232-236 --- The Chinese National Space Geodetic Network / J. Cai / pp. 237-240 --- Satellite Position Determination by Difference of Range (DOR) Measurements / I. Kardos / pp. 241-250 --- Recent Geodetic VLBI Results from Shanghai Observatory / Ye S., Qian Z., Chen G. and Zhou, R. / pp. 251-253 --- An Antennacluster-Antennacluster VLBI Project VERA / T. Sasao, N. Kawano, T. Hara, S. Kuji, K. Shibata, K. lwadate, K. Sato, 0. Kameya, S. Tsuruta, K. Asari, Y. Tamura, K. Horiai, K. Sato, H. Hanada, T. Tsubokawa, K. Yokoyama, S. Manabe and S. Sakai / pp. 254-258 --- An Astronomical Observational Plan Using the VERA / O. Kameya, T. Sasao, N. Kawano and K. M. Shibata / pp. 259-263 --- Estimated Errors in the Antennacluster-Antennacluster VLBI / T. Hara, T. Sasao, K. Sato, N. Kawano and O. Kameya / pp. 264-271 --- Sub-Milliarcsecond Astrometry with Phase-Referenced VLBI / D. L. Jones, J.-F. Lestrade, R. A. Preston and R. B. Phillips / pp. 272-276 --- Selenodesy by Using Differential VLBI Observations of Artificial Radio Sources on the Moon / H. Hanada, M. Ooe, N. Kawano, K. lwadate, S. Kuji, K. Sato, S. Tsuruta, T. Sasao, 0. Kameya, T. Hara, N. Kawaguchi, M. Fujishita, M. Morimoto, S. Yasuda, H. Mizutani and A. Fujimura / pp. 277-281 --- Gravitational Lens Effect and Measurement of Stellar Mass / M. Hosokawa, K. Ohnishi, T. Fukushima and M. Takeuti / pp. 282-286 --- Evidence for Source Structure Effects Caused by the Quasar 3C273 in Geodetic VLBI Data / P. Charlot / pp. 287-294 --- Astronomical Periods in the Solar System / Y. Macyama / pp. 295-305 --- Pulsar VLBI Experiment Using Kashima-Usuda Baseline / M. Sekido, S. Hama, H. Kiuchi, Y. Hanado, Y. Takahashi, M. Imae, K. Fujisawa and H. Hirabayashi / pp. 306-312 --- The Celestial Reference System and Frame of the International Earth Rotation Service / E. F. Arias / pp. 313-315 --- Quasi Simultaneous Observations in the Arclength Method of Reduction of Astrometric VLBI Data / M. S. De Biasi, E. F. Arias and J.-F. Lestrade / pp. 316-318 --- Few-Hundred Microarcsecond VLBI Astrometry: Applications and Reduction of Limiting Error Sources / S. T. Lowe and R. N. Treuhaft / pp. 319-323 --- Chapter 4. Recorders and Correlators --- A New Advanced One-Unit VLBI Correlator (NAOCO) / K. Shibata, T. Sasao, N. Kawaguchi, Y. Tamura, S. Kameno, M. Miyoshi, K. Asari, S. Manabe, T. Hara, S. Kuji, K. Sato, T. Miyaji, K. Matsumoto, Y. Asaki, S. Yasuda and S. Nakamura / pp. 327-331 --- A Programmable VLBI Correlator Using Parallel Computing / G. Petit and T. Fayard / pp. 332-337 --- Status of the New K-4 System / H. Kiuchi, S. Hama, J. Amagai, Y. Hanado, A. Kaneko and M. Imae / pp. 338-344 --- The S2 Frequency Agile Data Acquisition Terminal / W. T. Petrachenko, P. Mathieu, J. Popelar, W. H. Cannon, H. Tan and R. D. Wietfeldt / pp. 345-350 --- A Chipset for a MKII Style Correlator / G. Tuccari / pp. 351-359 --- Keeping Compatibility in International VLBI Systems / T. Yoshino, S. Hama and N. Kawaguchi / pp. 360-364 --- Development of the Burst Mode VLBI / K. Matsumoto and N. Kawaguchi / pp. 365-370 --- The K4 Correlator / S. Hama, H. Kiuchi, M. Sekido and M. Imae / pp. 371-376 --- Notes on High Data Rate Recording / J. Takayama / pp. 377-380

Description / Table of Contents: ing within the downgoing plate, and appears to be assoeiated with segmentation of the subdueting plate produeed by forees related to the subduetion of the Louisville Ridge. To analyze fault plane heterogeneities in the northern Solomon Islands subdue­ tion segment and their association with rupture eharaeteristics in general and the existenee of earthquake doublets in partieular, Xv and SCHWARTZ study in detail two sets of doublets, from 1974 and 1975, and then reloeate 85 underthrusting events in the area. The authors find that few smaller magnitude events overlap asperity regions, and that the majority of small magnitude underthrusting earth­ quak es oeeupy a segment that has never experieneed a magnitude greater than 7.0 earthquake in the historie times. It will be of great value to soeiety when seismologists and geophysieists are able to monitor and prediet the pattern of geophysieal phenomena assoeiated with subduetion; this issue presents a modest step towards this goal. PAGEOPH, Vol. 140, No. 2 (1993) 0033 ~4553;93;020 183 ~ 28$1.50 + 0.20;0 © 1993 Birkhäuser Verlag, Basel Slip Partitioning along Major Convergent Plate Boundaries 2 GUANG YU,l STEVEN G. WESNOUSKY,l and GÖRAN EKSTRÖM Abstract-Along plate boundaries characterized by oblique convergence, earthquake slip vectors are commonly rotated toward the normal of the trench with respect to predicted plate motion vectors. Consequently, relative plate motion along such convergent margins must be partitioned between displacements along the thrust plate interface and deformation within the foreare and back-are regions.

Description / Table of Contents: The 1957 great Aleutian earthquake.- The rupture process and tectonic implications of the great 1964 Prince William Sound earthquake.- Coseismic slip in the 1964 Prince William Sound earthquake A new geodetic inversion.- Seismicity trends and potential for large earthquakes in the Alaska-Aleutian region.- Rupture process of large earthquakes in the northern Mexico subduction zone.- Global variability in subduction thrust zone-forearc systems.- Large thrust earthquakes and volcanic eruptions.