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(Table 1) Refractive index of volcanic glass shards at DSDP Leg 56 Holes
Empty cells = not determined. Refractive index shows range, mean range, and mode of individual layers; range denotes the minimum and maximum refractive index, mean range is that... -
Interstitial water chemistry of Hole 56-436, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
Interstitial water chemistry of Hole 56-435A, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
Interstitial water chemistry of Hole 56-435, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
Interstitial water chemistry of Hole 56-434B, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
Interstitial water chemistry of Hole 56-434A, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
Interstitial water chemistry of Hole 56-434, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
(Table 1) Calculated paleoelevations of drillhole points 35 million years ago
This dataset has no description
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(Table 19) Distribution of radiolaria in Miocene to Pleistocene sediments of ...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
Geochemistry and geological ages for organic-rich black shales of the Quatern...
This dataset has no description
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Paleoelevations in the Pacific Ocean 35 million years ago
Data from deep sea drilling, linear magnetic anomalies and bathymetric measurements together with age and morphometric characteristics of seamounts have been used to construct a... -
Distribution of radiolaria in Oligocene to Pleistocene sediments of the North...
Neogene stratigraphy of the tropical and subtropical Pacific on radiolaria is studied in the book. A detailed comparison of coeval systems from tropics and subtropics is given.... -
Mineral and chemical compositions of clay sediments from the Pacific Ocean, D...
Mineral and chemical compositions, as well as conditions of formation of clay sediments in major structural elements of the Pacific Ocean floor with different ages are under... -
(Table 1) Major and trace elements at DSDP Leg 56 Holes
This dataset has no description
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(Table 50) Parameter b of clay minerals and polytypes of hydromica from sedim...
This dataset has no description
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(Table 48) Parameter b of clay minerals and polytypes of hydromica from sedim...
This dataset has no description
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(Table 46) Parameter b of clay minerals and polytypes of hydromica from sedim...
This dataset has no description
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Diatom abundance of Hole 56-436
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 56-434
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Ostracoda abundance of Hole 56-435
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
