Zobrazeno 1 - 10
of 19
pro vyhledávání: '"S.J. Pannalal"'
Publikováno v:
Geosphere. 8:1146-1169
Tectonic models for Borneo’s Cenozoic evolution differ in several aspects, particularly in the extent to which they include paleomagnetic data suggestive of strong counterclockwise rotation between 30 and 10 Ma. Key areas are undersampled. We prese
Publikováno v:
Journal of Geochemical Exploration. 106:188-196
The Upper Mississippi Valley (UMV) zinc–lead district contains archetypal examples of Mississippi Valley-type (MVT) ore deposits. Specimens (332) from 25 sites in the Lower Ordovician Oneota dolomite were collected from around the northern and east
Publikováno v:
Terra Nova. 20:385-393
Palaeomagnetism of 273 specimens from 24 sites isolated a well-defined characteristic remanent magnetization (ChRM) direction on AF and thermal demagnetization in seven host carbonate and 14 ore mineralization sites from the Galmoy Zn–Pb deposit. T
Publikováno v:
Journal of Geochemical Exploration. 89:309-313
Paleomagnetism (18 sites, 231 specimens) of Lower Carboniferous carbonates in Northern Ireland reveals three characteristic remanent magnetization (ChRM) components. Six sites from Brigantian limestones have a Middle Triassic (239 ± 7 Ma) secondary
Publikováno v:
Economic Geology. 100:295-309
Paleomagnetic results are reported from five Upper Mississippian and 19 Upper Pennsylvanian limestone and black shale sites (272 samples) and from 42 boulders, oriented with respect to their bedding, of Mississippi Valley-type (MVT) mineralization fr
Publikováno v:
Journal of Applied Geophysics. 56:135-153
The Upper Mississippi Valley (UMV) zinc–lead district of Wisconsin is located on the northern fringe of the Illinois basin. It was the first major Mississippi Valley-type (MVT) Zn–Pb district to be mined in the United States. Its mineralisation i
Publikováno v:
Journal of Geochemical Exploration. :235-241
Paleomagnetic analysis of 382 specimens from 27 sites in the Sweetwater Ba F Zn district in the southern AppalachianValley and Ridge province of eastern Tennessee indicates that peak dolomitisation or recrystallisation of the host rocks occurred duri
Autor:
D.T.A. Symons, S.J. Pannalal
Publikováno v:
Journal of Geochemical Exploration. 101:101
Publikováno v:
Journal of Geochemical Exploration. 90:215
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