Publications by authors named "F HOLTZ"

Article Synopsis
  • The Weilasituo Sn-polymetallic deposit in northeast China shows distinct mineralization zoning, including high-temperature Sn-W-Li minerals at the center and cooler Pb-Zn-Ag minerals at the edges.
  • Research using fluid inclusions and isotope studies aims to understand the genetic relationship and formation mechanism of these mineralizations, revealing the evolution of ore-forming fluids from high to low salinity and temperature over time.
  • Analysis indicates that early fluids had a magmatic origin, while later fluids integrated contributions from surrounding rocks and meteoric water, with distinct growth episodes of quartz linked to different fluid pulses.
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Syneruptive magma mixing is widespread in volcanic eruptions, affecting explosivity and composition of products, but its evidence in basaltic systems is usually cryptic. Here we report direct evidence of mixing between basanitic and tephritic magmas in the first days of the 2021 Tajogaite eruption of Cumbre Vieja, La Palma. Groundmass glass in tephritic tephra from the fifth day of the eruption is locally inhomogeneous, showing micron-scale filamentary structures of Si-poor and Fe-, Mg-rich melt, forming complex filaments attached to bubbles.

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Objective: This study aimed to identify the relevance of hospitalizations for congenital hip deformities in Bahia.

Methods: This is a retrospective epidemiological study in public databases. Descriptors in health sciences: "congenital hip dysplasia", "congenital hip dislocation", and "congenital dislocation hip".

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Basaltic crystal cargoes often preserve records of mantle-derived chemical variability that have been erased from their carrier liquids by magma mixing. However, the consequences of mixing between similarly primitive but otherwise chemically variable magmas remain poorly understood despite ubiquitous evidence of chemical variability in primary melt compositions and mixing-induced disequilibrium within erupted crystal cargoes. Here we report observations from magma-magma reaction experiments performed on analogues of primitive Icelandic lavas derived from distinct mantle sources to determine how their crystal cargoes respond to mixing-induced chemical disequilibrium.

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The determination of low boron concentrations in silicate glasses by electron probe microanalysis (EPMA) remains a significant challenge. The internal interferences from the diffraction crystal, i.e.

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