By John W. Hillhouse
About The Product
Published via the yankee Geophysical Union as a part of the Geophysical Monograph Series.
The inspiration of "accreted terranes," that continents develop via the addition of displaced fragments of crust, used to be the valuable subject of a contemporary multidisciplinary symposium subsidized by means of the foreign Union of Geodesy and Geophysics (IUGG). This quantity features a number of papers awarded in Symposium 12 at XIX common meeting of the IUGG, held August 15-18, 1987, in Vancouver. Convenors Edward Irving and David Stone centred this system on significant topics. the 1st was once to trace the displacement of terranes utilizing paleomagnetism, geologic mapping, and paleontology. the second one subject matter used to be to discover the deep constitution of accreted terranes utilizing seismological, geochemical, and potential-field tools. Given the scope of these issues, it's no shock that the individuals represented many specialties in the box of solid-earth geophysics. this system integrated case histories from a set of fold belts spanning a lot time and lengthy distances, from the Proterozoic sutures of North the USA to the Cenozoic accretionary complexes of the Pacific rim.
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Extra resources for Deep Structure and Past Kinematics of Accreted Terranes
Rundschau, 70, 583595, 1981. , Evidence of displaced terranes from Permian to Jurassic faunas around the Pacific margins, J. geol. Soc. London, 143, 209-216, - 1986. M. L. LaBrecque, W. T. J. Snelling, pp. 118-140, Geol. Soc. London Mem. 10, 1985. , Mesozoic California and the underflow of Pacific mantle, Geol. Soc. Amer. , 80, 2409-2430, 1969. Geophysical Monograph Series Deep Structure and Past Kinematics of Accreted Terranes Vol. S. Prof. Paper 1078, 1-345, 1979. B. S. G. Howell, pp. -Pac. Council Energy Min.
0 . -1 to r T. ■ .. Vol. 50 WILSON et al. 25 , 4 4 ► ▪ Geophysical Monograph Series Deep Structure and Past Kinematics of Accreted Terranes 26 GLOBAL MESOZOIC RECONSTRUCTIONS Paleotethys has been greatly reduced by subduction and ridge collision in the Central Asian area. Southwest Pacific Region The Gondwana margin remains much as it was in the Late Jurassic. West Irian Jaya, Obi-Bacan, Beru-Seram, Sabah and Panay-Mindoro have continued moving to the northwest, but now at a rate of some 15 cm/yr as estimated from sea floor data [Rea & Duncan, 1986].
D. McKenzie, pp. 17-24, Amer. Geophys. , 1987. , Manaslu leucogranite: a collision signature of the Himalaya, a model for its genesis and emplacement, J. Geophys. , 86B, 10,545-10,568, 1981. P. C. Ries, pp. 159-172, Geol. Soc. London Spec. Pub. 19, 1986. , Sea-floor spreading and continental drift, J. Geophys. , 73, 3661-3705, 1968. , The mixed Permian Cathaysia-Gondwana flora, The Palaeobotanist (Lucknow), 35, 211 222, 1986. Li, X. and Z. Yao, Discovery of Cathaysia flora in the Qinghai-Xizang Plateau with special reference to its Permian phytogeographical provinces, in Geological and Ecological Studies Of QinghaiXizang Plateau, Vol.
Deep Structure and Past Kinematics of Accreted Terranes by John W. Hillhouse