Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Mark A. Hutchison"'
Publikováno v:
The Astrophysical Journal, Vol 975, Iss 1, p 27 (2024)
We introduce the Contour Analysis Tool (CAT), a Python toolkit aimed at identifying and analyzing structural elements in density maps. CAT employs various contouring techniques, including the lowest-closed contour, linear and logarithmic Otsu thresho
Externí odkaz:
https://doaj.org/article/19748b5ed9374db8aade3c5f9731efba
Autor:
Cathie J. Clarke, Mark A. Hutchison
We model the gas and dust dynamics in a turbulent protoplanetary disc undergoing extreme-UV photoevaporation in order to better characterise the dust properties in thermal winds (e.g. size distribution, flux rate, trajectories). Our semi-analytic app
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a6c4d0624a0aace66dbd97576b6ffc4f
http://arxiv.org/abs/2011.08631
http://arxiv.org/abs/2011.08631
Autor:
Riccardo Reali, Gioacchino Tempesta, Mariangela Schiazza, Giovanna Agrosì, Paolo Nimis, Richard Spiess, Daniela Mele, D. Howell, Fabrizio Nestola, Mark T. Hutchison
Publikováno v:
Geology. 47:27-30
Publikováno v:
Mineralogy and petrology, 2018, Vol.112(S1), pp.115-132 [Peer Reviewed Journal]
The Glen Gollaidh aillikite dyke (58.36741°N 4.69751°W), N.W. Scotland, occurs within the Neoproterozoic sedimentary rocks of the Moine Supergroup ~4 km east of the Moine Thrust. Phlogopite 40Ar/36Ar measurements give a late Devonian maximum emplac
Autor:
Mark T. Hutchison
Publikováno v:
Mineralogy and Petrology. 112:737-753
Pre-1.6 Ga rocks comprise around 45% of the onshore area of Western Australia (WA), constituting the West Australian Craton (WAC) (including the Archean Yilgarn and Pilbara Cratons) and the western part of the North Australian Craton (NAC). These are
Publikováno v:
International Kimberlite Conference Extended Abstracts: 2008.
Dirk Frei, Mark T. Hutchison, Axel Gerdes and Larry M. Heaman Geological Survey of Denmark and Greenland, Ostervoldgade 10, DK-1350 Copenhagen K, Denmark (df@geus.dk) Johann Wolfgang Goethe Universitat, Institut fur Geowissenschaften, Altenhoferallee
Autor:
Mattia L. Mazzucchelli, Federica Marone, Matteo Alvaro, Simone Morganti, Mark T. Hutchison, Paolo Nimis, Chiara Anzolini, Andrea Gianese, Fabrizio Nestola, Jeff W. Harris, Marcello Campione
Publikováno v:
Geology
Super-deep diamonds (SDDs) are those that form at depths between ~300 and ~1000 km in Earth's mantle. They compose only 1% of the entire diamond population but play a pivotal role in geology, as they represent the deepest direct samples from the inte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e04637d3672c21e2b8ca7730d625a5b0
http://hdl.handle.net/10281/215811
http://hdl.handle.net/10281/215811
Autor:
Maria Cristina Caggiani, Annarosa Mangone, Gioacchino Tempesta, Daniela Mele, Giancarlo Della Ventura, Fabrizio Nestola, Mariangela Cestelli-Guidi, Paolo Nimis, Ignazio Allegretta, Giovanna Agrosì, Mark T. Hutchison
Super-deep diamonds and their mineral inclusions preserve very precious information about Earth’s deep mantle. In this study, we examined multiphase inclusions entrapped within a diamond from the Rio Vinte e um de Abril, Sao Luiz area (Juina, Brazi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ca569bf2fa264d098dfa4cc8f2d23ce9
http://hdl.handle.net/11577/3317246
http://hdl.handle.net/11577/3317246
Publikováno v:
Journal of morphology. 231(3)
This study of the morphology, histology, histochemistry, and ultrastructure of the Harderian gland in Geckos (Squamata, Gekkota) revealed previously unreported variation. The gecko Harderian gland is unlike that of other squamates in that each cell o
Autor:
Giovanna Agrosì, Mark T. Hutchison, Giancarlo Della Ventura, Fabrizio Nestola, Gioacchino Tempesta, Paolo Nimis, Mariangela Cestelli Guidi
Publikováno v:
Crystals, Vol 7, Iss 8, p 233 (2017)
Crystals; Volume 7; Issue 8; Pages: 233
Crystals; Volume 7; Issue 8; Pages: 233
Diamonds from Juina, Brazil, are well-known examples of superdeep diamond crystals formed under sublithospheric conditions and evidence would indicate their origins lie as deep as the Earth’s mantle transition zone and the Lower Mantle. Detailed ch