ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 160-970A; 160-971A; 160-971B; 160-971D; 160-971E; DRILL; Drilling/drill rig; Eastern Basin; Joides Resolution; Leg160; Ocean Drilling Program; ODP  (1)
  • PANGAEA  (1)
  • American Association of Petroleum Geologists
  • BioMed Central
Collection
Keywords
Publisher
  • PANGAEA  (1)
  • American Association of Petroleum Geologists
  • BioMed Central
Years
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Schulz, Hans-Martin; Emeis, Kay-Christian; Volkmann, N (1997): Organic carbon provenance and maturity in the mud breccia from the Napoli mud volcano: Indicators of origin and burial depth. Earth and Planetary Science Letters, 147(1-4), 141-151, https://doi.org/10.1016/S0012-821X(97)00013-7
    Publication Date: 2024-01-09
    Description: Mud volcanism on the Mediterranean Ridge is caused by extrusion of overpressured sediments, with consequent formation of spectacular dome-shaped features composed of mud breccias at the seafloor. The organic material in the mud breccia of the Napoli mud volcano is a mixture of different facies, stratigraphic origin and thermal maturities. One portion is synsedimentary organic material with only minor diagenetic alterations and represents sedimenting material that was embedded into the mud volcano during its extrusion. The mud breccia also contains thermally mature organic material of mainly terrestrial provenance with algae of fresh- and brackish-water origin. Vitrinite reflectance data of this maturity generation range from 0.65 to 0.90% R(oil) and thus characterize thermally mature source rocks, a rank which is corroborated by fluorescence and molecular characteristics. The predominance of vitrinite in the maceral assemblages and the occurrence of biomarkers of terrigenous origin suggest that the major part of the mud matrix derives from a lacustrine or riverine sedimentary unit in the subsurface, possibly from the Messinian stage. A third generation of organic material includes inertinites and vitrinites of high reflectance, which represent recycled organic matter present in any marine sediment. By use of the Lopatin method for modelling the thermal maturation of hydrocarbon source rocks from the vitrinite reflectance data, we calculated that the depth of mobilization ranges from 4900 m to 7500 m, depending upon the temperature gradient used.
    Keywords: 160-970A; 160-971A; 160-971B; 160-971D; 160-971E; DRILL; Drilling/drill rig; Eastern Basin; Joides Resolution; Leg160; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...