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(Table 1) Major and trace element and isotopic composition of ODP Leg 129 ign...
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(Table T5) Paleomagnetic properties of igneous samples from ODP Site 129-800,...
Sediment depth is given in mbsf. Note that for 129-800-57R polarity assumed normal; for Cores 129-800-58R and 129-800-60R polarity assumed reversed. -
(Table 6) Mass accumulation rates for Jurassic to early Cretaceous sediments ...
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(Table 6) Chemistry of radiolarite samples from ODP Sites 129-801 and 129-800
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(Table 3) Chemical analyses of igneous rocks from ODP Hole 129-801C
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(Table 1) Physical properties of igneous rocks from ODP Leg 129 sites
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(Appendix) Demagnetization steps of ODP Hole 129-801C basalts
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(Table 1) Paleomagnetic analyses of ODP Hole 129-801C basalts
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(Appendix) Demagnetization steps of ODP Hole 129-802A samples
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(Table 1) Paleomagnetic analyses of ODP Hole 129-802A
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(Table 3) Oxygen and carbon isotopic composition of carbonates and silicates ...
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(Table 2) Chemical analyses of the hydrothermal deposit and interpillow mater...
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(Table 1) Chemistry of secondary phyllosilicates in ODP Hole 129-801C basement
Structural formulas calculated on the basis of O10(OH)2. -
(Table 5) Incremental heating and age determination of whole-rock samples fro...
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(Table 4) Incremental heating and age determination for whole-rock samples fr...
1100°C = heat each of the previously heated basalt fragments to 1100°C, measure individually. Fuse previously heated basalt fragments, measure in three groups of three fragments... -
(Table 3) Incremental heating and age determination for mineral separates fro...
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(Table 2) Incremental heating and age determination for mineral separates fro...
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(Table 1) Summary of ODP Leg 129 basalts age determinations
Best Age: 129-800A = 126.1 ± 0.6 Ma; 129-801 alkalic basalts = 157.4 ± 0.5 Ma; 129-801C tholeiitic basalts = 166.8 ± 4.5 Ma; 12-802A = 114.6 ± 3.2 Ma. -
(Table 4) Chemical analyses of basaltic rocks from ODP Hole 129-801C
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(Table 3) Chemical analyses of basaltic rocks from ODP Hole 129-801B
This dataset has no description