HFSE

AcronymDefinition
HFSEHigh Field Strength Elements (chemistry)
HFSEHigh Field Strength Element
HFSEHigh Frequency Somatic Embryogenesis
HFSEHigh Frequency Seismic Element
HFSEHeart Failure Screening Echo
HFSEHigh Frequency Somatic Embryos
References in periodicals archive ?
HFSE 2011 will be held at the Navy Pier in Chicago, September 20-22, 2011.
Xie and Kerrich (1994) inferred that the trace-element signamres, particularly the ratios of HFSE (Zr, Hf, Nb) to the REE can distinguish between olivine (shallow mantle), majorite (>14 GPa; > ~ 400 km; Herzberg 1995) and perovskite (lower mantle) fractionation.
With respect to HFSE, Hurricane samples are not consistently more or less abundant than the Boil Mountain samples, although Hurricane Mountain samples are depleted in HREE (Fig.
HFSE organizers also raised a record $9,600 during the conference, for Access Community Health Network, Chicago's largest private primary health care provider to the underserved and the nation's largest community health center organization.
Bringing together the professionals who design, plan, construct and manage healthcare facilities, HFSE uses expert sessions and features focused on major trends and challenges at the forefront of the industry to help educate their attendees and keep them tapped into the latest news impacting their facilities and businesses.
This andesite is highly enriched in LREE and LFSE, and highly depleted in HFSE relative to MORB (Figs.
The addition of workshops like the 'Exploring the Manufacturability of Healthcare Environments' is how HFSE is continuing to be the place the entire industry comes together to solve the problems of today and plan the facilities of tomorrow.
Suites (1) through (4) display incremental increases in absolute trace-element abundances, though all, except the andesitic basalt, are characterized by low HFSE contents.
Trace-element systematics suggest derivation from a mantle source that was enriched in HFSE compared to normal MORB, prior to introduction of Th and LILE via metasomatizing fluids from the subducting slab.
The REE and HFSE data for basalts from the Clementine West area are tholeiitic and completely unlike the typical Buchans River Formation.
REE and HFSE data also suggest that spatial geochemical variations occur in the PQR itself In the Lucky Strike area, the PQR has the most enriched Th and Zr anomalies of all samples analysed.