Crystallography Open Database

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Searching journal of publication like 'Journal of Mineralogical and Petrological Sciences' volume of publication is 103

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1544852 CIFAl9.21 Ca3.64 H50.4 K0.4 Na1.14 O97.2 Si26.88 Sr0.21C 1 2/m 117.716; 17.78; 7.438
90; 116.43; 90
2098Khobaer, T.M.; Kuribayashi, T.; Komatsu, K.; Kudoh, Y.
The partially dehydrated structure of natural heulandite: An in situ high temperature single crystal X-ray diffraction study Sample: room temperature
Journal of Mineralogical and Petrological Sciences, 2008, 103, 61-76
1544853 CIFAl9.21 Ca3.64 H50.4 K0.4 Na1.14 O97.2 Si26.88 Sr0.21C 1 2/m 117.694; 17.801; 7.433
90; 116.41; 90
2096.8Khobaer, T.M.; Kuribayashi, T.; Komatsu, K.; Kudoh, Y.
The partially dehydrated structure of natural heulandite: An in situ high temperature single crystal X-ray diffraction study Sample: 100 C
Journal of Mineralogical and Petrological Sciences, 2008, 103, 61-76
1544854 CIFAl9.21 Ca3.64 H50.4 K0.4 Na1.14 O97.2 Si26.88 Sr0.21C 1 2/m 117.725; 17.63; 7.459
90; 116.79; 90
2080.7Khobaer, T.M.; Kuribayashi, T.; Komatsu, K.; Kudoh, Y.
The partially dehydrated structure of natural heulandite: An in situ high temperature single crystal X-ray diffraction study Sample: 150 C
Journal of Mineralogical and Petrological Sciences, 2008, 103, 61-76
1544855 CIFAl9.21 Ca3.64 H50.4 K0.4 Na1.14 O97.2 Si26.88 Sr0.21C 1 2/m 117.716; 17.584; 7.452
90; 116.7; 90
2073.9Khobaer, T.M.; Kuribayashi, T.; Komatsu, K.; Kudoh, Y.
The partially dehydrated structure of natural heulandite: An in situ high temperature single crystal X-ray diffraction study Sample: 200 C
Journal of Mineralogical and Petrological Sciences, 2008, 103, 61-76
1544856 CIFAl9.21 Ca3.64 H50.4 K0.4 Na1.14 O97.2 Si26.88 Sr0.21C 1 2/m 117.082; 16.685; 7.351
90; 116.93; 90
1867.9Khobaer, T.M.; Kuribayashi, T.; Komatsu, K.; Kudoh, Y.
The partially dehydrated structure of natural heulandite: An in situ high temperature single crystal X-ray diffraction study Sample: 250 C
Journal of Mineralogical and Petrological Sciences, 2008, 103, 61-76

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