Andrea Giuliani

ORCID: 0000-0002-6823-2807
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About
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Research Areas
  • Geological and Geochemical Analysis
  • earthquake and tectonic studies
  • High-pressure geophysics and materials
  • Geochemistry and Geologic Mapping
  • Gastric Cancer Management and Outcomes
  • Geology and Paleoclimatology Research
  • Mineralogy and Gemology Studies
  • Hydrocarbon exploration and reservoir analysis
  • Helicobacter pylori-related gastroenterology studies
  • Geological Studies and Exploration
  • Colorectal Cancer Surgical Treatments
  • Geological and Geophysical Studies
  • Colorectal Cancer Screening and Detection
  • Urological Disorders and Treatments
  • Genetic factors in colorectal cancer
  • Urinary and Genital Oncology Studies
  • Gastrointestinal Tumor Research and Treatment
  • Metastasis and carcinoma case studies
  • Clay minerals and soil interactions
  • Diverticular Disease and Complications
  • Antimicrobial Peptides and Activities
  • Geological and Geophysical Studies Worldwide
  • Multiple and Secondary Primary Cancers
  • Methane Hydrates and Related Phenomena
  • Gastrointestinal disorders and treatments

Carnegie Institution for Science
2024-2025

ETH Zurich
2019-2024

Institute of Geochemistry
2019-2024

Istituto di Astrofisica Spaziale e Fisica Cosmica di Milano
2023

Sapienza University of Rome
2001-2022

The University of Melbourne
2013-2022

Policlinico Umberto I
2006-2022

Macquarie University
2015-2020

Australian Research Council
2015-2020

ARC Centre of Excellence for Core to Crust Fluid Systems
2016-2020

Ore deposits are loci on Earth where energy and mass flux greatly enhanced focussed, acting as magnifying lenses into metal transport, fractionation concentration mechanisms through the lithosphere. Here we show that metallogenic architecture of lithosphere is illuminated by geochemical signatures metasomatised mantle rocks post-subduction magmatic-hydrothermal mineral systems. Our data reveal anomalously gold tellurium rich magmatic sulfides in mantle-derived magmas emplaced lower crust...

10.1038/s41467-019-11065-4 article EN cc-by Nature Communications 2019-08-05

Kimberlites represent magmas derived from great mantle depths and are the principal source of diamonds. their xenolith cargo have been extremely useful for determining chemical composition, melting regime evolution subcontinental mantle. The late-Devonian Udachnaya (means Fortuitous) pipe hosts largest diamond deposit in Russia (> 60% quantity value) one world, supplying gem-quality diamonds (~ 12% world production). Since its discovery 1956, kimberlite has become a "type locality"...

10.1016/j.earscirev.2014.09.004 article EN cc-by-nc-nd Earth-Science Reviews 2014-09-22

Quantifying the compositional evolution of mantle-derived melts from source to surface is fundamental for constraining nature primary and deep Earth composition. Despite abundant evidence interaction between carbonate-rich melts, including diamondiferous kimberlites, mantle wall rocks en route surface, effects this on melt compositions are poorly constrained. Here, we demonstrate a robust linear correlation Mg/Si ratios kimberlites their entrained components Mg/Fe olivine cores magmatic rims...

10.1126/sciadv.aaz0424 article EN cc-by-nc Science Advances 2020-04-24

Mantle polymict breccias sampled by kimberlite magmas are complex mixtures of mantle minerals and rock clasts, cemented together olivine, phlogopite, orthopyroxene, ilmenite, rutile sulphides. Because the kimberlite-like texture (i.e. mineral clasts diverse origin composition set in a magmatic matrix) large geochemical heterogeneity preserved breccias, these rocks believed to derive from primitive or precursor magmas. Therefore, study such xenoliths can provide constraints on processes...

10.1093/petrology/egu008 article EN Journal of Petrology 2014-03-11

Kimberlites and orangeites (previously named Group-II kimberlites) are small-volume igneous rocks occurring in diatremes, sills dykes. They the main hosts for diamonds of scientific importance because they contain fragments entrained mantle crustal rocks, thus providing key information about subcontinental lithosphere. Orangeites ultrapotassic, H2O CO2-rich hosting minerals such as phlogopite, olivine, calcite apatite. The major, trace element isotopic compositions resemble those intensely...

10.1038/ncomms7837 article EN cc-by-nc-nd Nature Communications 2015-04-17

Hypabyssal kimberlites are subvolcanic intrusive rocks crystallised from mantle-derived magmas poor in SiO2 and rich CO2 H2O. They complex, hybrid containing significant amounts of fragments, primarily olivine with rare diamonds, set a matrix essentially magmatic origin. Unambiguous identification requires careful petrographic examination combined mineral compositional analyses. Melt inclusion studies have shown that kimberlite melts contain higher alkali concentrations than previously...

10.2138/gselements.15.6.381 article EN Elements 2019-12-01

Abstract Magmatic systems play a crucial role in enriching the crust with volatiles and elements that reside primarily within Earth’s mantle, including economically important metals like nickel, copper platinum-group elements. However, transport of these silicate magmas occurs dense sulfide liquids, which tend to coalesce, settle not be efficiently transported ascending magmas. Here we show textural observations, backed up carbon oxygen isotope data, indicate an intimate association between...

10.1038/s41467-020-18157-6 article EN cc-by Nature Communications 2020-08-28

In-situ RbSr dating of mica by laser ablation ICP-MS/MS has recently emerged as a new tool to date range geological processes including magmatic, metamorphic and hydrothermal events. The majority age results presented are based on Rb/Sr calibration using the MicaMG pressed nano-powder pellet. However, some studies have reported low accuracy associated with ages this method, which attributed different properties natural mica. In work, we document systematic comparison between isotope-dilution...

10.1016/j.chemgeo.2024.121982 article EN cc-by Chemical Geology 2024-02-07

A large 10-mer phage peptide library was panned against whole Escherichia coli cells, and an antimicrobial (QEKIRVRLSA) selected. The synthesized in monomeric dendrimeric tetrabranched form (multiple antigen [MAP]), which generally allows a dramatic increase of stability to peptidases proteases. antibacterial activity the E. much higher than that form. Modification original sequence, by residue substitution or sequence shortening, produced three different MAPs, M4 (QAKIRVRLSA), M5...

10.1128/aac.49.7.2665-2672.2005 article EN Antimicrobial Agents and Chemotherapy 2005-06-25

Research Article| November 01, 2012 Nature of alkali-carbonate fluids in the sub-continental lithospheric mantle A. Giuliani; Giuliani 1School Earth Sciences, University Melbourne, Parkville, 3010 Victoria, Australia Search for other works by this author on: GSW Google Scholar V.S. Kamenetsky; Kamenetsky 2ARC Centre Excellence on Ore Deposits, and School Tasmania, Hobart, 7001 D. Phillips; Phillips M.A. Kendrick; Kendrick Australia3Wyatt Geological Consulting Ltd, 1/3 Westbury Grove, East...

10.1130/g33221.1 article EN Geology 2012-08-23

In response to the need for new antiviral agents, dendrimer-based molecules have been recognized as having a large number of potential therapeutic applications. They include peptide-derivatized dendrimers, which are hyperbranched synthetic well-defined consist peptidyl branching core and covalently attached surface functional peptides. However, few studies addressed their applications direct-acting agents. Here, we report on ability peptide dendrimer SB105 its derivative, SB105_A10, directly...

10.1128/aac.00149-11 article EN Antimicrobial Agents and Chemotherapy 2011-05-17

Kimberlites are rare, enigmatic, low-volume igneous rocks. They highly enriched in magnesium, volatiles (CO2 and H2O) incompatible trace elements thought to be the most deeply derived (>150 km) magmatic rocks on Earth. occur ancient thick continental lithosphere, forming intrusive sheets composite pipes, commonly clusters. Despite their rarity, kimberlites have attracted considerable attention because they entrain not only abundant mantle fragments but also diamonds, which can provide...

10.2138/gselements.15.6.377 article EN Elements 2019-12-01

Significance Understanding how the Earth evolved from its accretion to present-day conditions is a major quest of sciences. This contribution focuses on evolution deepest realms our planet sampled by basalts in ocean islands (such as Hawaii) during last ∼100 150 million years and diamond-bearing kimberlites emplaced continents since ∼2 billion ago. Radiogenic isotope ratios are employed demonstrate that these lavas share common source, which includes component originated melt extraction soon...

10.1073/pnas.2015211118 article EN Proceedings of the National Academy of Sciences 2020-12-23
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