TY - JOUR A1 - Beaulieu, Jean-Philippe A1 - Bennett, David P. A1 - Fouqué, Pascal A1 - Williams, Andrew A1 - Dominik, Martin A1 - Jorgensen, Uffe Grae A1 - Kubas, Daniel A1 - Cassan, Arnaud A1 - Coutures, Christian A1 - Greenhill, John A1 - Hill, Kym A1 - Menzies, John A1 - Sackett, Penny D. A1 - Albrow, Michael D. A1 - Brillant, Stephane A1 - Caldwell, John A. R. A1 - Calitz, Johannes Jacobus A1 - Cook, Kem H. A1 - Corrales Cosmeli, Esperanza de Santa Cecilia A1 - Desort, Morgan A1 - Dieters, Stefan A1 - Dominis, Dijana A1 - Donatowicz, Jadzia A1 - Hoffman, Martie A1 - Kane, Stephen R. A1 - Marquette, Jean-Baptiste A1 - Martin, Ralph A1 - Meintjes, Pieter A1 - Pollard, Karen R. A1 - Sahu, Kailash C. A1 - Vinter, Christian A1 - Wambsganss, Joachim A1 - Woller, Kristian A1 - Horne, Keith A1 - Steele, Iain A1 - Bramich, Daniel M. A1 - Burgdorf, Martin A1 - Snodgrass, Colin A1 - Bode, Mike A1 - Udalski, Andr T1 - Discovery of a cool planet of 5.5 Earth masses through gravitational microlensing N2 - In the favoured core-accretion model of formation of planetary systems, solid planetesimals accumulate to build up planetary cores, which then accrete nebular gas if they are sufficiently massive. Around M-dwarf stars ( the most common stars in our Galaxy), this model favours the formation of Earth-mass (M+) to Neptune-mass planets with orbital radii of 1 to 10 astronomical units (AU), which is consistent with the small number of gas giant planets known to orbit M-dwarf host stars(1-4). More than 170 extrasolar planets have been discovered with a wide range of masses and orbital periods, but planets of Neptune's mass or less have not hitherto been detected at separations of more than 0.15 AU from normal stars. Here we report the discovery of a 5.5(-2.7)(+5.5)M(+) planetary companion at a separation of 2.6(- 0.6)(+1.5) AU from a 0.22(-0.11)(+0.21)M(.) M-dwarf star, where M-. refers to a solar mass. (We propose to name it OGLE- 2005-BLG-390Lb, indicating a planetary mass companion to the lens star of the microlensing event.) The mass is lower than that of GJ876d (ref. 5), although the error bars overlap. Our detection suggests that such cool, sub-Neptune-mass planets may be more common than gas giant planets, as predicted by the core accretion theory. Y1 - 2006 UR - http://www.nature.com/nature/ U6 - https://doi.org/10.1038/Nature04441 SN - 0028-0836 ER - TY - JOUR A1 - Kubas, Daniel A1 - Cassan, A. A1 - Beaulieu, Jean-Philippe A1 - Coutures, C. A1 - Dominik, M. A1 - Albrow, Michael D. A1 - Brillant, Stephane A1 - Caldwell, John A. R. A1 - Dominis, Dijana A1 - Donatowicz, J. A1 - Fendt, Christian A1 - Fouque, P. A1 - Jorgensen, Uffe Grae A1 - Greenhill, John A1 - Hill, K. A1 - Heinmüller, Janine A1 - Horne, Keith A1 - Kane, Stephen R. A1 - Marquette, Jean-Baptiste A1 - Martin, Ralph A1 - Menzies, J. W. A1 - Pollard, K. R. A1 - Sahu, K. C. A1 - Vinter, C. A1 - Wambsganss, Joachim A1 - Watson, R. A1 - Williams, A. A1 - Thurl, C. T1 - Full characterization of binary-lens event OGLE-2002-BLG-069 from PLANET observations N2 - We analyze the photometric data obtained by PLANET and OGLE on the caustic-crossing binary-lens microlensing event OGLE-2002-BLG-069. Thanks to the excellent photometric and spectroscopic coverage of the event, we are able to constrain the lens model up to the known ambiguity between close and wide binary lenses. The detection of annual parallax in combination with measurements of extended-source effects allows us to determine the mass, distance and velocity of the lens components for the competing models. While the model involving a close binary lens leads to a Bulge- Disc lens scenario with a lens mass of M = (0.51 ± 0.15) M-&ODOT; and distance of D-L = (2.9 ± 0.4) kpc, the wide binary lens solution requires a rather implausible binary black-hole lens ( M &GSIM; 126 M-&ODOT;). Furthermore we compare current state-of-the-art numerical and empirical models for the surface brightness profile of the source, a G5III Bulge giant. We find that a linear limb-darkening model for the atmosphere of the source star is consistent with the data whereas a PHOENIX atmosphere model assuming LTE and with no free parameter does not match our observations Y1 - 2005 SN - 0004-6361 ER - TY - JOUR A1 - Cassan, A. A1 - Beaulieu, Jean-Philippe A1 - Brillant, Stephane A1 - Coutures, C. A1 - Dominik, M. A1 - Donatowicz, J. A1 - Jorgensen, Uffe Grae A1 - Kubas, Daniel A1 - Albrow, Michael D. A1 - Caldwell, John A. R. A1 - Fouque, P. A1 - Greenhill, John A1 - Hill, K. A1 - Horne, Keith A1 - Kane, Stephen R. A1 - Martin, Ralph A1 - Menzies, J. W. A1 - Pollard, K. R. A1 - Sahu, K. C. A1 - Vinter, C. A1 - Wambsganss, Joachim A1 - Watson, R. A1 - Williams, A. A1 - Fendt, Christian A1 - Hauschildt, P. A1 - Heinmueller, Janine A1 - Marquette, Jean-Baptiste A1 - Thurl, C. T1 - Probing the atmosphere of the bulge G5III star OGLE-2002-BUL-069 by analysis of microlensed H alpha line N2 - We discuss high-resolution, time-resolved spectra of the caustic exit of the binary microlensing event OGLE 2002-BLG-069 obtained with UVES on the VLT. The source star is a G5III giant in the Galactic Bulge. During such events, the source star is highly magnified, and a strong differential magnification around the caustic resolves its surface. Using an appropriate model stellar atmosphere generated by the PHOENIX v2.6 code we obtain a model light curve for the caustic exit and compare it with a dense set of photometric observations obtained by the PLANET microlensing follow up network. We further compare predicted variations in the Halpha equivalent width with those measured from our spectra. While the model and observations agree in the gross features, there are discrepancies suggesting shortcomings in the model, particularly for the Halpha line core, where we have detected amplified emission from the stellar chromosphere after the source star's trailing limb exited the caustic. This achievement became possible by the provision of the very efficient OGLE-III Early Warning System, a network of small telescopes capable of nearly-continuous round-the-clock photometric monitoring, on-line data reduction, daily near-real-time modelling in order to predict caustic crossing parameters, and a fast and efficient response of a 8 m class telescope to a "Target-of-Opportunity" observation request Y1 - 2004 ER - TY - JOUR A1 - Jiang, G. F. A1 - DePoy, D. L. A1 - Gal-Yam, A. A1 - Gaudi, B. S. A1 - Gould, A. A1 - Han, C. A1 - Lipkin, Y. A1 - Maoz, D. A1 - Ofek, E. O. A1 - Park, B. G. A1 - Pogge, R. W. A1 - Udalski, A. A1 - Kubiak, Marcin A1 - Szymanski, M. K. A1 - Szewczyk, O. A1 - Zerbrun, K. A1 - Wyrzykowski, L. A1 - Soszynski, I. A1 - Pietrzynski, G. A1 - Albrow, Michael D. A1 - Beaulieu, Jean-Philippe A1 - Caldwell, John A. R. A1 - Cassan, A. A1 - Coutures, C. A1 - Dominik, M. A1 - Donatowicz, J. A1 - Fouque, P. A1 - Greenhill, John A1 - Hill, K. A1 - Horne, Keith A1 - Jorgensen, S. F. A1 - Jorgensen, Uffe Grae A1 - Kane, Stephen R. A1 - Kubas, Daniel A1 - Martin, Ralph A1 - Menzies, J. W. A1 - Pollard, R. A1 - Sahu, K. C. A1 - Wambsganss, Joachim A1 - Watson, R. A1 - Williams, A. T1 - OGLE-2003-BLG-238 : Microlensing mass estimate of an isolated star N2 - Microlensing is the only known direct method to measure the masses of stars that lack visible companions. In terms of microlensing observables, the mass is given by M (c(2)/4G)(r) over tilde (E)theta(E) and so requires the measurement of both the angular Einstein radius theta(E) and the projected Einstein radius (r) over tilde (E). Simultaneous measurement of these two parameters is extremely rare. Here we analyze OGLE-2003-BLG-238, a spectacularly bright (I-min 10.3), high-magnification (A(max) 170) microlensing event. Pronounced finite-source effects permit a measurement of theta(E) = 650 muas. Although the timescale of the event is only t(E) 38 days, one can still obtain weak constraints on the microlens parallax: 4.4 AU < <(r)over tilde>(E) < 18 AU at the 1 σ level. Together these two parameter measurements yield a range for the lens mass of 0.36 M-&ODOT; < M < 1.48 M-&ODOT;. As was the case for MACHO- LMC-5, the only other single star (apart from the Sun) whose mass has been determined from its gravitational effects, this estimate is rather crude. It does, however, demonstrate the viability of the technique. We also discuss future prospects for single-lens mass measurements Y1 - 2004 SN - 0004-637X ER - TY - JOUR A1 - Sackett, Penny D. A1 - Albrow, Michael D. A1 - Beaulieu, Jean-Philippe A1 - Caldwell, John A. R. A1 - Coutures, C. A1 - Dominik, M. A1 - Greenhill, John A1 - Hill, K. A1 - Horne, Keith A1 - Jorgensen, Uffe Grae A1 - Kane, Stephen R. A1 - Kubas, Daniel A1 - Martin, Ralph A1 - Menzies, J. W. A1 - Pollard, K. R. A1 - Sahu, K. C. A1 - Wambsganß, Joachim A1 - Watson, R. A1 - Williams, A. T1 - PLANET II : a microlensing and transit search for extrasolar planets N2 - Due to their extremely small luminosity compared to the stars they orbit, planets outside our own Solar System are extraordinarily difficult to detect directly in optical light. Careful photometric monitoring of distant stars, however, can reveal the presence of exoplanets via the microlensing or eclipsing effects they induce. The international PLANET collaboration is performing such monitoring using a cadre of semi-dedicated telescopes around the world. Their results constrain the number of gas giants orbiting 1-7 AU from the most typical stars in the Galaxy. Upgrades in the program are opening regions of ''exoplanet discovery space'' - toward smaller masses and larger orbital radii - that are inaccessible to the Doppler velocity technique. Y1 - 2003 UR - http://arxiv.org/pdf/astro-ph/0211098 ER - TY - JOUR A1 - Toy, Virginia Gail A1 - Sutherland, Rupert A1 - Townend, John A1 - Allen, Michael J. A1 - Becroft, Leeza A1 - Boles, Austin A1 - Boulton, Carolyn A1 - Carpenter, Brett A1 - Cooper, Alan A1 - Cox, Simon C. A1 - Daube, Christopher A1 - Faulkner, D. R. A1 - Halfpenny, Angela A1 - Kato, Naoki A1 - Keys, Stephen A1 - Kirilova, Martina A1 - Kometani, Yusuke A1 - Little, Timothy A1 - Mariani, Elisabetta A1 - Melosh, Benjamin A1 - Menzies, Catriona D. A1 - Morales, Luiz A1 - Morgan, Chance A1 - Mori, Hiroshi A1 - Niemeijer, Andre A1 - Norris, Richard A1 - Prior, David A1 - Sauer, Katrina A1 - Schleicher, Anja Maria A1 - Shigematsu, Norio A1 - Teagle, Damon A. H. A1 - Tobin, Harold A1 - Valdez, Robert A1 - Williams, Jack A1 - Yeo, Samantha A1 - Baratin, Laura-May A1 - Barth, Nicolas A1 - Benson, Adrian A1 - Boese, Carolin A1 - Célérier, Bernard A1 - Chamberlain, Calum J. A1 - Conze, Ronald A1 - Coussens, Jamie A1 - Craw, Lisa A1 - Doan, Mai-Linh A1 - Eccles, Jennifer A1 - Grieve, Jason A1 - Grochowski, Julia A1 - Gulley, Anton A1 - Howarth, Jamie A1 - Jacobs, Katrina A1 - Janku-Capova, Lucie A1 - Jeppson, Tamara A1 - Langridge, Robert A1 - Mallyon, Deirdre A1 - Marx, Ray A1 - Massiot, Cécile A1 - Mathewson, Loren A1 - Moore, Josephine A1 - Nishikawa, Osamu A1 - Pooley, Brent A1 - Pyne, Alex A1 - Savage, Martha K. A1 - Schmitt, Doug A1 - Taylor-Offord, Sam A1 - Upton, Phaedra A1 - Weaver, Konrad C. A1 - Wiersberg, Thomas A1 - Zimmer, Martin T1 - Bedrock geology of DFDP-2B, central Alpine Fault, New Zealand JF - New Zealand journal of geology and geophysics : an international journal of the geoscience of New Zealand, the Pacific Rim, and Antarctica ; NZJG N2 - During the second phase of the Alpine Fault, Deep Fault Drilling Project (DFDP) in the Whataroa River, South Westland, New Zealand, bedrock was encountered in the DFDP-2B borehole from 238.5–893.2 m Measured Depth (MD). Continuous sampling and meso- to microscale characterisation of whole rock cuttings established that, in sequence, the borehole sampled amphibolite facies, Torlesse Composite Terrane-derived schists, protomylonites and mylonites, terminating 200–400 m above an Alpine Fault Principal Slip Zone (PSZ) with a maximum dip of 62°. The most diagnostic structural features of increasing PSZ proximity were the occurrence of shear bands and reduction in mean quartz grain sizes. A change in composition to greater mica:quartz + feldspar, most markedly below c. 700 m MD, is inferred to result from either heterogeneous sampling or a change in lithology related to alteration. Major oxide variations suggest the fault-proximal Alpine Fault alteration zone, as previously defined in DFDP-1 core, was not sampled. KW - Alpine Fault KW - New Zealand KW - scientific drilling KW - mylonite KW - cataclasite Y1 - 2017 U6 - https://doi.org/10.1080/00288306.2017.1375533 SN - 0028-8306 SN - 1175-8791 VL - 60 IS - 4 SP - 497 EP - 518 PB - Taylor & Francis CY - Abingdon ER -