Zobrazeno 1 - 10
of 36
pro vyhledávání: '"Maria A. Mange"'
Autor:
Maria A. Mange, Fu-Yuan Wu, Qing-Zhu Yin, Q. Zhou, Y. Liu, John F. Dewey, Josh Wimpenny, Xian-Hua Li, Qiu-Li Li, G.-Q. Tang, D. L. Tollstrup
Publikováno v:
Journal of the Geological Society. 169:681-689
Ordovician strata of the South Mayo Trough in western Ireland contain clastic deposits that represent materials eroded from a large and diverse continental area over a time scale that spans much of the Earth’s history. Therefore, it is a useful reg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c238ea2a59244bde7041c3c9f0aadaae
https://doi.org/10.1144/jgs2011-164
https://doi.org/10.1144/jgs2011-164
Autor:
Asish R. Basu, Junsheng Nie, Carmala N. Garzione, Brian K. Horton, Mauricio Parra, Andrés Mora, Victor Caballero, Joel E. Saylor, Christopher J. Moreno, Maria A. Mange
Publikováno v:
Earth-Science Reviews. 110:111-126
article i nfo Sediment provenance analysis remains a powerful method for testing hypotheses on the temporal and spatial evolution of uplifted source regions, but issues such as recycling, nonunique sources, and pre- and post- depositional modificatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::77e5a67a2f1ad9d1fbce203862bb15d1
https://doi.org/10.1016/j.earscirev.2011.11.002
https://doi.org/10.1016/j.earscirev.2011.11.002
Publikováno v:
Journal of the Geological Society. 167:1147-1160
The Ordovician strata of the South Mayo Trough in western Ireland were deposited as a conformable sequence, first in the forearc of a north-facing oceanic arc, then in a synorogenic basin above the arc–continent collisional Grampian orogen, then in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a566d85ebdea81377941518d5fc2f2a4
https://doi.org/10.1144/0016-76492009-091
https://doi.org/10.1144/0016-76492009-091
Autor:
Tam´s Bezeczky, Maria A. Mange
Publikováno v:
Geoarchaeology. 21:429-460
Amphorae sherds from the Laecanius workshop of Roman Istria (10–5 B.C. and 78 A.D.), Croatia, were studied by integrating archaeological and geological techniques including fabric analysis, thin-section petrography, X-ray diffractometry (XRD), and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f4ed174e9ac9aa12d4487d75a9bcb513
https://doi.org/10.1002/gea.20115
https://doi.org/10.1002/gea.20115
Autor:
Maria A. Mange, Ervin G. Otvos
Publikováno v:
Sedimentary Geology. 182:29-57
High Resolution Heavy Mineral Analysis (HRHMA) of late Pleistocene terrace samples, their Tertiary source rocks, and modern river sediments provided an effective tool for reconstructing sediment provenance and mapping heavy mineral provinces in south
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1fd822b4161012dbdb5ec6b34640540
https://doi.org/10.1016/j.sedgeo.2005.07.015
https://doi.org/10.1016/j.sedgeo.2005.07.015
Publikováno v:
Proceedings of the Geologists' Association. 116:251-280
The heavy mineral components of Ordovician greywacke turbidites of the Southern Uplands (subduction-accretion prism) Terrane were studied using high-resolution heavy mineral analysis. Diagnostic heavy minerals and the discovery of hitherto unreported
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::27756ef35b8c261c2bca3d01daf4ae3c
https://doi.org/10.1016/s0016-7878(05)80045-8
https://doi.org/10.1016/s0016-7878(05)80045-8
Publikováno v:
Tectonophysics. 384:91-113
Collision of the oceanic Lough Nafooey Island Arc with the passive margin of Laurentia after 480 Ma in western Ireland resulted in the deformation, magmatism and metamorphism of the Grampian Orogeny, analogous to the modern Taiwan and Miocene New Gui
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c8ceea74064460eb8a5a6b7750bc9ad
https://doi.org/10.1016/j.tecto.2004.03.009
https://doi.org/10.1016/j.tecto.2004.03.009
Publikováno v:
Geological Society, London, Special Publications. 221:97-110
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ec49cc1723590b8e6e13f1213e795a69
https://doi.org/10.1144/gsl.sp.2004.221.01.06
https://doi.org/10.1144/gsl.sp.2004.221.01.06
Publikováno v:
Geological Magazine. 140:25-30
Heavy minerals in Ordovician successions in western Ireland record, in the Upper Arenig Sheeffry Formation, the erosion of an ophiolite/island arc complex. The appearance of staurolite and garnet at a basin-wide horizon in the Lower Llanvirn Upper De
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::989a62830e54e035c10769edd367d4cb
https://doi.org/10.1017/s0016756802007100
https://doi.org/10.1017/s0016756802007100
Autor:
Jeremy Preston, Maria A. Mange-Rajetzky, Adrian J. Hartley, Lee Vaughan, Malcolm J. Hole, Steve Buck, Geoff May
Publikováno v:
Journal of Sedimentary Research. 72:18-29
A geochemical study of the heavy-mineral suite in Triassic strata from two wells in the Beryl Embayment was undertaken in order to identify changes in provenance through the Lewis Formation. Detailed provenance studies also allow the reconstruction o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a116a56cdddf0e7aebb3d870eaa9597b
https://doi.org/10.1306/042201720018
https://doi.org/10.1306/042201720018