Milankovitch climate cycles in ODP wireline logs
Conference
·
OSTI ID:6591704
Orbitally induced climatic rhythms can cause cyclical variations in the physical properties or mineralogy of deep-sea sediments. Regional variations in the climatic factors controlling sedimentation (e.g., rainfall, temperature, or current patterns) are likely to cause regional variations in the mineralogic signature of Milankovitch orbital cycles. Downhold geophysical logs, routinely recorded during ODP, continuously sample changes in sediment properties and mineralogy with depth. Thus, logs form an important methodology for detecting these changes and have the potential of indicating the local sedimentary response to the Milankovitch forcing functions. Cores lack a complete stratigraphic record of the well because of incomplete core recovery. The log, however, returns a continuous set of measurements every 15 cm with standard logs and eery 1.5 cm with neutron activation logs, allowing one to extend the study of Milankovitch cycles to older sediments than are accessible by core analyses. Examples of Milankovitch cycles in logs are available from the Labrador Sea (ODP Site 646), Baffin Bay (ODP site 645), Weddell Sea (ODP Sit 693), and Oman Margin (Leg 117). Porosity variations for sediments at ODP Site 646 (9-2Ma) and ODP Site 693 (8-4.5 Ma) indicate major periods of 90,000-110,000 years and 40,000-45,000 years, concordant with the periods of eccentricity and obliquity. In contrast, at ODP Site 645 (3.0-1.8 Ma) the dominant periods are eccentricity and 19,000-23,000 years (precession). The introduction of logging tools with higher vertical resolution in the near future will permit this type of study to be extended to sites with lower sedimentation rates.
- OSTI ID:
- 6591704
- Report Number(s):
- CONF-880301-
- Country of Publication:
- United States
- Language:
- English
Similar Records
Lower cretaceous organic-rich sediments drilled on Antarctic continental margin during ODP Leg 113
Lower Cretaceous organic-rich sediments drilled on Antarctic Continental Margin during ODP Leg 113
Seismic stratigraphy, Cenozoic basin evolution, and sedimentary history of the southern part of Baffin Bay, Canada: preliminary results of ODP Leg 105
Conference
·
Thu Dec 31 23:00:00 EST 1987
·
OSTI ID:5924157
Lower Cretaceous organic-rich sediments drilled on Antarctic Continental Margin during ODP Leg 113
Conference
·
Sun Jan 31 23:00:00 EST 1988
· AAPG Bull.; (United States)
·
OSTI ID:5794308
Seismic stratigraphy, Cenozoic basin evolution, and sedimentary history of the southern part of Baffin Bay, Canada: preliminary results of ODP Leg 105
Conference
·
Fri May 01 00:00:00 EDT 1987
· AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
·
OSTI ID:5785271
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