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Geosynclines is devoted to the geosynclines concept, which states that the most elevated parts of the earth's crust—the mountains—had risen by a gigantic inversion of relief from the more depressed regions where they had originated. This book re-examines the concept in light of further geological evidence. The book is organized into four parts. Part I presents a detailed account of the birth and development of the geosynclinal concept. It shows that only the European (Alpine) concept of the geosyncline involves a fundamental palaeogeographical differentiation of mountain chains, and that it is from this standpoint that the American concept must be considered if it is to be placed in a more general framework. Part II attempts to define the geosynclinal concept in the Alpine sense of the term: i.e., in the light of current views on the Mediterranean chains of the Alpine cycle, which are the best documented. Part III collates the information acquired on the various aspects of geosynclines as exemplified by the Mediterranean chains of the Alpine cycle. Part IV discusses the degree to which the ""Alpine"" concept of the geosyncline may be extended in time.
This book covers advances in the methods of catalytic asymmetric synthesis and their applications. Coverage moves from new materials and technologies to homogeneous metal-free catalysts and homogeneous metal catalysts. The applications of several methodologies for the synthesis of biologically active molecules are discussed. Part I addresses recent advances in new materials and technologies such as supported catalysts, supports, self-supported catalysts, chiral ionic liquids, supercritical fluids, flow reactors and microwaves related to asymmetric catalysis. Part II covers advances and milestones in organocatalytic, enzymatic and metal-based mediated asymmetric synthesis, including applications for the synthesis of biologically active molecules. Written by leading international experts, this book consists of 16 chapters with 2000 References and illustrations of 560 schemes and figures.
Through a remarkable combination of intellect, self-confidence, engaging humility, and prodigious output of published work, William R. Dickinson influenced and challenged three generations of sedimentary geologists, igneous petrologists, tectonicists, sandstone petrologists, archaeologists, and other geoscientists. A key figure in the plate-tectonic revolution of the 1960s and 1970s, he explained how the distribution of sediments on Earth's surface could be traced to tectonic processes, and is widely recognized as a founder of modern sedimentary basin analysis. This volume consists of 31 chapters related to Dickinson's research interests; many of the authors are his former students, their students, and their students' students, demonstrating his continuing profound influence. The papers in this volume are an impressive tribute to the depth and breadth of Bill Dickinson's contributions to the geosciences.