Results 91 to 100 of about 13,826 (203)
(Table 4) Chemical composition of pyroxene at DSDP Site 57-438
(Table 4) Chemical composition of pyroxene at DSDP Site 57 ...
Fujioka, Kantaro +5 more
core +1 more source
Trace element composition of silicate minerals from Kunashak Meteorite (L6)
Major (EPMA) and trace (SIMS) element geochemistry in the silicate minerals (olivine, pyroxene and plagioclase) of Kunashak equilibrated ordinary chondrite (L6) is described. No variations in the major element concentrations of the silicate minerals have
Kristina G. Sukhanova, Olga L. Galankina
doaj
Low-temperature heat capacities (5-330 K) have been measured by adiabatic calorimetry for synthetic caAl2sio6 glass and pyroxene. The values of siq.15 -s$ are 155.3 J/mol . K for the glass and 135.3 J/mol ' K for the pyroxene. These entropies do not
B S Hetuttncway +3 more
core
(Table 6) Major element composition of pyroxene DSDP Hole 67-495
(Table 6) Major element composition of pyroxene DSDP Hole 67 ...
R C Maury (6962147) +13 more
core +1 more source
(Table 9) Trace elements of pyroxene of ODP Leg 135 vitrophyric rhyolite samples
(Table 9) Trace elements of pyroxene of ODP Leg 135 vitrophyric rhyolite ...
Ewart, Anthony +3 more
core +1 more source
In this paper based on new petrochemical and geochemical data with specificity in the compositions of rock-forming and ore minerals were determine the conditions of formation of Ti-Fe-V mineralization in the two-pyroxene gabbro of Medvedevskoje deposit ...
V. V. Holodnov +3 more
doaj +2 more sources
(Table 2) Chemical composition of pyroxene from DSDP Hole 89-462A
(Table 2) Chemical composition of pyroxene from DSDP Hole 89 ...
Castillo, Paterno R +5 more
core +1 more source
(Table 4) Alkali pyroxene analyses from alkalic basalts from ODP Site 129-801
(Table 4) Alkali pyroxene analyses from alkalic basalts from ODP Site 129 ...
Rowbotham, G +3 more
core +1 more source
Magnetic Imaging of the Effect of Stress on the Remanent Magnetization of Basalt
Abstract Differential compressional stresses (<100 MPa) that do not result in permanent deformation have traditionally been considered insufficient to modify paleomagnetic signals; however, recent numerical predictions have challenged this assumption.
A. R. Muxworthy +7 more
wiley +1 more source
Trace elements in the silicate minerals of the Borodino Meteorite (Н5)
Major (EPMA) and trace (SIMS) element geochemistry in olivine, low-Са pyroxene and mesostasis from porphyritic and barred chondrules, as well as the pyroxene-olivine aggregate and matrix of equilibrated ordinary Borodino chondrite (Н5) is discussed. No
Kristina G. Sukhanova
doaj

