1![Toshitaka Uchino T. Hyodo, M. Oka 1
The possible bound state of the Kbar nuclei attracts much attention. Among Toshitaka Uchino T. Hyodo, M. Oka 1
The possible bound state of the Kbar nuclei attracts much attention. Among](https://www.pdfsearch.io/img/e6eb062196ce4420b6a8cb9ab5c38a70.jpg) | Add to Reading ListSource URL: www.phys.kyushu-u.ac.jpLanguage: English - Date: 2012-08-20 02:56:12
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2![FB20 in Fukuoka , 20-25 August, 2012 Year : 2012 Kbar-Hyperon Interactions and Possible S-wave Resonances FB20 in Fukuoka , 20-25 August, 2012 Year : 2012 Kbar-Hyperon Interactions and Possible S-wave Resonances](https://www.pdfsearch.io/img/c359e1df75989faf182e816c3c95702f.jpg) | Add to Reading ListSource URL: www.phys.kyushu-u.ac.jpLanguage: English - Date: 2012-08-20 00:30:10
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3![](https://www.pdfsearch.io/img/df694cf3e9de22757608475bae7d712f.jpg) | Add to Reading ListSource URL: www.deepseadrilling.orgLanguage: English - Date: 2007-05-10 11:11:00
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4![High-pressure metamorphism during the Llano orogeny inferred from Proterozoic eclogite remnants Amy Wilkerson, William D. Carlson, Douglas Smith Department of Geological Sciences, University of Texas, Austin, Texas 78713 High-pressure metamorphism during the Llano orogeny inferred from Proterozoic eclogite remnants Amy Wilkerson, William D. Carlson, Douglas Smith Department of Geological Sciences, University of Texas, Austin, Texas 78713](https://www.pdfsearch.io/img/82c287711195e92538d25fad91eacf1f.jpg) | Add to Reading ListSource URL: www.geo.utexas.eduLanguage: English - Date: 2009-07-13 14:29:13
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5![I v American Mineralogist, Volume 79, pages, 1994 Nearly pure iron staurolite in the Llano Uplift and its petrologic significance I v American Mineralogist, Volume 79, pages, 1994 Nearly pure iron staurolite in the Llano Uplift and its petrologic significance](https://www.pdfsearch.io/img/d001fd6c0eafa278f0e3ae57f28c6a5a.jpg) | Add to Reading ListSource URL: www.geo.utexas.eduLanguage: English - Date: 2009-07-13 14:29:14
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6![Paris Edinburgh cell 100 kbar [Th. Straessle et al] PSI information day’09 33 Paris Edinburgh cell 100 kbar [Th. Straessle et al] PSI information day’09 33](https://www.pdfsearch.io/img/9977ca465bcefecd895e1ecd47c22040.jpg) | Add to Reading ListSource URL: www.psi.ch- Date: 2015-03-05 09:17:35
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7![clamp cells for 9 and 14 kbar PSI information day’09 32 clamp cells for 9 and 14 kbar PSI information day’09 32](https://www.pdfsearch.io/img/cefeadd15573d31289378e89240c9719.jpg) | Add to Reading ListSource URL: www.psi.ch- Date: 2015-03-05 09:17:35
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8![Fadenquarze von der Kluft Z 16 sind bei einer Temperatur von 340° bis 360°C und einem Druck von 3 bis 3.4 Kbar entstanden. Dieser Druck entspricht einer Felsüberlagerung von 9 bis 12 km (je nach Dichte des Gesteins). Fadenquarze von der Kluft Z 16 sind bei einer Temperatur von 340° bis 360°C und einem Druck von 3 bis 3.4 Kbar entstanden. Dieser Druck entspricht einer Felsüberlagerung von 9 bis 12 km (je nach Dichte des Gesteins).](https://www.pdfsearch.io/img/5c57bd88bab66b1846c0c1b4faced058.jpg) | Add to Reading ListSource URL: www.kristalle.chLanguage: German - Date: 2011-08-04 16:10:42
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9![Paris Edinburgh cell 100 kbar [Th. Straessle et al] PSI information day’09 33 Paris Edinburgh cell 100 kbar [Th. Straessle et al] PSI information day’09 33](https://www.pdfsearch.io/img/4feb154a8ad27abc84f8586b123f2f6b.jpg) | Add to Reading ListSource URL: sinq.web.psi.ch- Date: 2009-11-20 07:50:19
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10![clamp cells for 9 and 14 kbar PSI information day’09 32 clamp cells for 9 and 14 kbar PSI information day’09 32](https://www.pdfsearch.io/img/1c1c8ae0a81da8bc2776a77f689c17e4.jpg) | Add to Reading ListSource URL: sinq.web.psi.ch- Date: 2009-11-20 07:53:17
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