Oxygen isotope variation of granites and marbles in the vicinity of the shizhuyuan super giant W-Sn-Mo-Bi Ore Deposit, Hunan, P.R.China

1998 ◽  
Vol 43 (S1) ◽  
pp. 50-50
Author(s):  
Guo Xinsheng
2008 ◽  
Vol 68 (1) ◽  
pp. 187-218 ◽  
Author(s):  
E. D. Young ◽  
K. Kuramoto ◽  
R. A. Marcus ◽  
H. Yurimoto ◽  
S. B. Jacobsen

2009 ◽  
Vol 54 (16) ◽  
pp. 2758-2765 ◽  
Author(s):  
Jing Gao ◽  
LiDe Tian ◽  
YongQin Liu ◽  
TongLiang Gong

2004 ◽  
Vol 68 (6) ◽  
pp. 1253-1263 ◽  
Author(s):  
David L. Dettman ◽  
Karl W. Flessa ◽  
Peter D. Roopnarine ◽  
Bernd R. Schöne ◽  
David H. Goodwin

2008 ◽  
pp. 187-218 ◽  
Author(s):  
Edward D. Young ◽  
Kyoshi Kuramoto ◽  
Rudolph A. Marcus ◽  
Hisayoshi Yurimoto ◽  
Stein B. Jacobsen

Science ◽  
2006 ◽  
Vol 313 (5794) ◽  
pp. 1763-1765 ◽  
Author(s):  
R. C. Greenwood

2011 ◽  
Vol 90 (2-3) ◽  
pp. 259-270 ◽  
Author(s):  
H.B. Vonhof ◽  
J.W.M. Jagt ◽  
A. Immenhauser ◽  
J. Smit ◽  
Y.W. van den Berg ◽  
...  

AbstractBelemnitellid cephalopods from the Maastrichtian stratotype area (southeast Netherlands) are shown to be comparatively well preserved. Although partial diagenetic alteration has been observed, micromilling techniques have permitted the extraction of pristine belemnite calcite, suitable for the reconstruction of strontium (Sr), oxygen (O) and carbon (C) isotope variation of Maastrichtian seawater. A distinct Sr isotope pattern in the Maastricht record can be matched stratigraphically with records from Hemmoor (northern Germany), El Kef (Tunisia) and ODP site 690 (Maud Rise, Antarctica), leading to a new chemostratigraphical age model for the Maastrichtian stratotype section. Our data improve currently applied strontium isotope stratigraphical reference curves by revealing an Sr isotope inflection pattern near the lower/upper Maastrichtian boundary that is a potentially diagnostic feature for intra-Maastrichtian stratigraphical correlation between distant sections. Belemnites further show significant stratigraphical oxygen isotope variation through the Maastrichtian. We interpret this variation to have resulted from palaeoceanographic reorganisations in the Atlantic Ocean during this time interval.


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