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Tectonic Evolution, Collision, and Seismicity of Southwest Asia
Southwest Asia is one of the most remarkable regions on Earth in terms of active faulting and folding, large-magnitude earthquakes, volcanic landscapes, petroliferous foreland basins, historical civilizations as well as geologic outcrops that display the protracted and complex 540 m.y. stratigraphic record of Earth's Phanerozoic Era. Emerged from the birth and demise of the Paleo-Tethys and Neo-Tethys oceans, southwest Asia is currently the locus of ongoing tectonic collision between the Eurasia-Arabia continental plates. The region is characterized by the high plateaus of Iran and Anatolia fringed by the lofty ranges of Zagros, Alborz, Caucasus, Taurus, and Pontic mountains; the region also includes the strategic marine domains of the Persian Gulf, Gulf of Oman, Caspian, and Mediterranean. This 19-chapter volume, published in honor of Manuel Berberian, a preeminent geologist from the region, brings together a wealth of new data, analyses, and frontier research on the geologic evolution, collisional tectonics, active deformation, and historical and modern seismicity of key areas in southwest Asia.
Sedimentary Basin Tectonics from the Black Sea and Caucasus to the Arabian Platform
This wide area of the Alpine-Himalayan belt evolved through a series of tectonic events related to the opening and closure of the Tethys Ocean. In doing so it produced the largest mountain belt of the world, which extends from the Atlantic to the Pacific oceans. The basins associated with this belt contain invaluable information related to mountain building processes and are the locus of rich hydrocarbon accumulations. However, knowledge about the geological evolution of the region is limited compared to what they offer.
Feldspar Minerals
33 14. 3. 5 REE between Plagioclase and Aqueous Fluid 0 Cullers et al. (1973) measured the distribution of REE at 850 C and 750 bars pressure between a natural plagioclase, An , and gaseous water. The rare earths 65 favored the plagioclase by a factor which varies from about 25 for Ce to 10 for Lu. Data were also obtained for forsterite, diopside, enstatite and two rhyolite glasses, on the one hand, and water on the other hand, thereby permitting estimation of the partition coefficients between all pairs of phases. 14. 4 Chemical Substitution in Natural Feldspars 14. 4. 1 Introduction It is quite impracticable to give all the data on chemical substitution in natural feldspars: indeed many of...
Glioblastoma:
Glioblastoma is the most malignant brain tumor that still remains incurable. It is such a deadly disease that patients do not survive more than a few months after diagnosis. Our understanding of the histopathology and molecular mechanisms of formation of glioblastoma is rapidly advancing so as to provide us clues for devising rational therapeutic strategies for treatment of this malignancy. It is important that we continue to improve our knowledge about the pathogenesis of this devastating disease and explore new areas to find successful therapeutic strategies. Various approaches such as sophisticated imaging techniques, improved surgical procedures, ground-breaking strategies for radiotherapy, chemotherapy, immunotherapy, chemoimmunotherapy, and photodynamic therapy are being used for eradicating glioblastoma. Hopefully, this book will be an important source of information on glioblastoma and therefore be highly useful to the students, postdoctoral fellows, principal investigators, and clinicians involved in this field.
Rock-Forming Minerals
This part deals mainly with the disilicates and ring silicates including the epidote, melilite, cordierite and tourmaline groups. In addition to the minerals dealt with in the first edition, some of the rarer but typical minerals in the calc-silicate rocks and the accessory minerals of nepheline-syenites and related rocks have been included. The orthosilicates, in particular the olivine, garnet and humite groups are covered in Volume 1A.
