9 10 This paper makes a review of the interpretations of the tectonic evolution of SW Japan 11 during the last three decades. In the late 1970s, the dominant model was the so-called 12 ―Pacific-type orogeny‖, emphasizing the purported absence of nappes and the contrast with 13 the alpine chains, and interpreting the evolution as due to a steady oceanic subduction since 14 the Paleozoic time. In...

9 10 This paper makes a review of the interpretations of the tectonic evolution of SW Japan 11 during the last three decades. In the late 1970s, the dominant model was the so-called 12 ―Pacific-type orogeny‖, emphasizing the purported absence of nappes and the contrast with 13 the alpine chains, and interpreting the evolution as due to a steady oceanic subduction since 14 the Paleozoic time. In...

Both single and multigrain U-Pb zircon thermal ionization mass spectrometry (TIMS) as well as sensitive high resolution ion microprobe (SHRIMP ll) dating of two suites of Adirondack granites have yielded ages constraining the principal tectonomagmatic events of the Ottawan Orogeny to the interval ca 1090–1035 Ma. The earliest of these consists of mildly A-type hornblende granites of the Hawkeye...

The Pacific margin of East Antarctica records a long tectonic history of crustal growth and breakup, culminating in the early Paleozoic Ross Orogeny associated with Gondwanaland amalgamation. Periods of older tectonism have been proposed (e.g. Precambrian Nimrod and Beardmore Orogenies), but the veracity of these events is difficult to document because of poor petrologic preservation, geochrono...