This book details the immense impact that Jorge Luis Borges has had on the thinking and writing of the twentieth century and how many have misunderstood that impact. It highlights how his symbols, techniques, parody, irony, and artful ambiguity in his fiction, essays, and poems force us to question what we can know with certainty, what is real and what is dream, and who we are, and thus define what has become the core of the postmodern vision. The book explores Borges's distinctly Latin American postmodern pluralism. It details how this pluralism has informed the postmodern discussions of the self, love, history, feminism, and politics, and has influenced writers in the U.S. and Latin America. Throughout, it argues that the Argentine writer avoids the nihilism and chaos of a radical relativism that many have come to associate with postmodernism. Rather, his vision affirms values and a search for positive knowledge. Mark Frisch is Associate Professor in the Department of Modern Languages and Literatures at Duquesne University.
The Island of Syros (Cyclades, Greece) is a prime locality for the study of processes active in deep levels of orogens and is world famous for its exceptionally well preserved blueschist- to eclogite-facies lithologies. Syros Island was completely remapped at a scale of 1:25,000. Detailed lithostratigraphical observations and area-wide, closely spaced structural measurements allowed a much more detailed depiction of the highly variable lithological assemblage, as well as of the complex structural evolution. Lithostratigraphical indications, such as the distribution of Mn-mineralization and sequential repetition of characteristic marker successions, suggest that the whole-rock pile of the Cycladic Blueschist Unit on Syros, including meta-ophiolites and metasediments, retains numerous primary depositional features. Magmatic activity in an Upper Cretaceous backarc environment was likely to be contemporaneous with the deposition of the sedimentary protoliths comprising the main lithological succession on Syros. The structural evolution of the Cycladic Blueschist Unit on Syros comprises multiphase isoclinal intrafolial folding and ductile thrusting, regarded as essentially burial related and terminating close to peak metamorphic conditions, either prograde or very early on the retrograde path. Especially in areas where blueschist- to eclogite-facies metamorphism is undisturbed, high-pressure fabrics are well preserved. The retrograde evolution was accompanied by heterogeneously distributed, weakly developed extensional tectonics and episodical, contractional deformation, followed by intense brittle transpressional and transtensional tectonics, disrupting the rock sequence since Miocene to subrecent times.
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