Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Barbara M. Hill"'
Autor:
Penelope J. Lancaster, Barbara M. Hill, M.E. Bickford, Bin Fu, James M. McLelland, Noriko T. Kita, F. Z. Page, John W. Valley
Publikováno v:
Journal of Metamorphic Geology. 27:41-54
Oxygen isotope ratios and rare earth element (REE) concentrations provide independent tests of competing models of injection v. anatexis for the origin of migmatites from amphibolite and granulite facies metasedimentary rocks of the Adirondack Mounta
Publikováno v:
Chemical Geology. 256:24-32
Subduction of the Pacific plate beneath the Mariana forearc releases fluids to the overlying mantle wedge that ascend, producing serpentinite “mud” that discharges on the ocean floor. As part of Leg 195 of the Ocean Drilling Program cores were ob
Publikováno v:
Geological Society of America Bulletin. 120:950-961
U-Pb sensitive high-resolution ion microprobe (SHRIMP) analyses of zircons from migmatitic metapelites in the eastern Adirondack Highlands demonstrate that substantial anatexis took place ca. 1050 Ma during the late, but still high-grade, ca. 1090–
Autor:
Matthew J. Heumann, Michael J. Jercinovic, Barbara M. Hill, James M. McLelland, Bruce Selleck, M.E. Bickford
Publikováno v:
Geological Society of America Bulletin. 118:1283-1298
Anatectic leucogranites are common in metapelites within both the highlands and lowlands terranes of the Adirondack Mountains of northern New York State. The formation of these igneous bodies, which are folded in the lowlands and commonly mylonitized
Autor:
Barbara M. Hill, M.E. Bickford, John W. Valley, Michael A. Hamilton, Cory C. Clechenko, James M. McLelland
Publikováno v:
Geological Society of America Bulletin. 116:1299-1317
The low abundance of igneous zircon in Proterozoic massif anorthosites has presented a major obstacle to the acquisition of direct absolute ages of crystallization for these important rocks. Indirect dating that relies on zircon ages from associated
Publikováno v:
Canadian Journal of Earth Sciences. 38:1017-1025
An augened, strongly flasered, and multiply folded monzonitic gneiss occurs in a structural dome in the Black Bear Island Lake region of northern Saskatchewan, within the ca. 1850 Ma Paleoproterozoic southern Rottenstone Domain of the Trans-Hudson Or
Publikováno v:
Nursing Clinics of North America. 27:1-10
Autor:
Donald I. Siegel, Barbara M. Hill
Publikováno v:
Journal of Hydrology. 123:211-224
Variations in the concentrations of metals in three peat profiles from the Lost River Peatland, Minnesota are related to the degree of groundwater discharge into the peat, rather than the metal content of the peat when it was originally deposited. El
Publikováno v:
Geology. 36:555
Lu-Hf depleted mantle model (TDM) ages, obtained by analysis of zircons previously dated by U-Pb methods, demonstrate that ca. 1.75 Ga bimodal Paleoproterozoic rocks in the Gunnison-Salida region of central Colorado, and by extension in much of the s
Autor:
Barbara M. Hill, M.E. Bickford
Publikováno v:
Geology. 35:167
A common model for the Paleoproterozoic crustal evolution of southern Laurentia involves southerly accretion of successively younger island arcs from 1780 to 1650 Ma. This model may be oversimplified, however, for although andesite and basaltic andes