Abstract
Time–depth relationships (TDR) are required for correlating geological information from drill sites with seismic reflection profiles. Conventional time–depth domain conversion is implemented using P-wave velocity data, derived from downhole sonic logs, calibrated with vertical seismic check-shots. During scientific ocean drilling expeditions, immediate seismic correlation is carried out using laboratory velocities measured on recovered core material. As these three velocity measurements vary significantly in signal frequency, resolution and acoustic pathways, they carry potential for substantial TDR differences and consequent miscorrelation to seismic profiles. Our analytical work uses the comprehensive scientific ocean drilling dataset to quantify these differences in core-seismic integration. TDRs are calculated and compared at sites where check-shot, sonic log, and laboratory velocity measurements cover the same depth segments of the drill hole. We find that the maximum differences between the TDRs (TDR \(diff_{max}\)) reach up to 55%, which can cause fundamental errors in the seismic correlation. No direct relationship to porosity and bulk density of the cored material is observed. Instead, higher TDR variability is found at sites with carbonate content > 70%, particularly with coarser grain texture. Sites containing primarily igneous and siliciclastic sequences show less than 10% TDR \(diff_{max}\). This semi-quantitative criterion indicates that downhole logging should be conducted during drilling expeditions, especially at sites with carbonate sequences, or low core recovery, to ensure accurate core-seismic integrations.
Similar content being viewed by others
References
Amante C, Eakins BW (2009) ETOPO1 1 arc-minute global relief model: procedures, data sources and analysis. http://www.ngdcnoaagov/mgg/global/globalhtml. https://doi.org/10.7289/v5c8276m
Ballard MS, Lee K (2017) The acoustics of marine sediments. Acoust Today 13:11–18
Bartel DC, Busby M, Nealon J, Zaske J (2006) Time to depth conversion and uncertainty assessment using average velocity modeling. In: SEG Technical Program Expanded Abstracts 2006. Society of Exploration Geophysicists, pp 2166–2170. https://doi.org/10.1190/1.2369965
Biot MA (1956a) Theory of propagation of elastic waves in a fluid-saturated porous solid. I. Low-frequency range. J Acoust Soc Am 28:168–178. https://doi.org/10.1121/1.1908239
Biot MA (1956b) Theory of propagation of elastic waves in a fluid-saturated porous solid. II. Higher frequency range. J Acoust Soc Am 28:179–191. https://doi.org/10.1121/1.1908241
Blum P (1997) Physical properties handbook: a guide to the shipboard measurement of physical properties of deep-sea cores. ODP Tech, College Station
Carlson R, Gangi A, Snow K (1986) Empirical reflection travel time versus depth and velocity versus depth functions for the deep-sea sediment column. J Geophys Res 91:8249–8266. https://doi.org/10.1029/JB091iB08p08249
Del Grosso VA (1974) New equation for the speed of sound in natural waters (with comparisons to other equations). J Acoust Soc Am 56:1084–1091. https://doi.org/10.1121/1.1903388
Dunham RJ (1962) Classification of carbonate rocks according to depositional textures. In: Ham WE (ed) Classification of carbonate rocks. AAPG, Tulsa, pp 108–121
Dushaw BD, Worcester PF, Cornuelle BD, Howe BM (1993) On equations for the speed of sound in seawater. J Acoust Soc Am 93:255–275
Eberli GP et al (1997) Proceedings of the Ocean Drilling Program, initial reports; Bahamas Transect, covering Leg 166 of the cruises of the Drilling Vessel JOIDES Resolution, San Juan, Puerto Rico, to Balboa Harbor, Panama, sites 1003–1009, 17 Feb–10 Apr 1996. Texas A & M University, Ocean Drilling Program, College Station, TX, USA. https://doi.org/10.2973/odp.proc.ir.166.1997
Eberli GP, Baechle GT, Anselmetti FS, Incze ML (2003) Factors controlling elastic properties in carbonate sediments and rocks. Lead Edge 22:654–660. https://doi.org/10.1190/1.1599691
Feary DA, Hine AC, James NP, Malone MJ (2004) Leg 182 synthesis: exposed secrets of the Great Australian Bight. In: Proceedings of the Ocean Drilling Program, Scientific Results, pp 1–30. https://doi.org/10.2973/odp.proc.ir.182.2000
Fulthorpe CS, Schlanger SO, Jarrard RD (1989) In situ acoustic properties of pelagic carbonate sediments on the Ontong Java Plateau. J Geophys Res 94:4025–4032. https://doi.org/10.1029/JB094iB04p04025
Goetz J, Dupal L, Bowler J (1979) An investigation into discrepancies between sonic log and seismic check spot velocities. APPEA J 19:131–141. https://doi.org/10.1071/AJ78014
Hamilton EL (1976) Shear-wave velocity versus depth in marine sediments: a review. Geophysics 41:985–996. https://doi.org/10.1190/1.1440676
Hamilton EL (1980) Geoacoustic modeling of the sea floor. J Acoust Soc Am 68:1313–1340. https://doi.org/10.1121/1.385100
Harvey PK, Lovell MA (1998) Core-log integration controls (Special Publications). Geological Society, London, p 136
IODP International Ocean Discovery Program Database. http://iodp.org/resources/access-data-and-samples. Accessed 2017–2018
Isern A, Anselmetti F, Blum P (2002) Proceedings of the Ocean Drilling Program. Initial Reports Leg 194. College Station, TX (Ocean Drilling Program). https://doi.org/10.2973/odp.proc.ir.194.2002
Lowrie W (1997) Fundamental of geophysics. Cambridge University Press, Cambridge
Maturi E, Sapper J, Harris A, Mittaz J (2014) GHRSST level 4 OSPO global foundation sea surface temperature analysis (GDS version 2). National Oceanographic Data Center, NOAA, Dataset. https://doi.org/10.7289/v5sq8xfh. Accessed 2017–2018
Moore CH, Wade WJ (2013) Carbonate reservoirs: porosity and diagenesis in a sequence stratigraphic framework, vol 67. Elsevier, Amsterdam
Mutter J, Balch A (1988) Vertical Seismic Profiling (VSP) and the Ocean Drilling Program (ODP): Report of a Workshop. Joint Oceanogr. Inst./US Science Advisory Comm.
NASA (2015) Aquarius Official Release Level 3 Sea Surface Salinity Standard Mapped Image Monthly Data V4.0., 4.0. edn. https://doi.org/10.5067/aqr40-3smcs
Neto IdAL, Misságia RM (2012) Estimate of elastic properties including pore geometry effect on carbonates: a case study of Glorieta-Paddock reservoir at Vacuum field, New Mexico. Revista Brasileira de Geofísica 30:519–532
Pälike H, Lyle M, Nishi H, Raffi I, Gamage K, Klaus A (2010) The expedition 320/321 scientists. In: Proceedings of the Integrated Ocean Drilling Program, p 321. https://doi.org/10.2204/iodp.proc.320321.2010
Pedley HM, Carannante G (2006) Cool-water carbonates: depositional systems and palaeoenvironmental. Geological Society of London, London
Pike J, Beiboer F (1993) A comparison between algorithms for the speed of sound in seawater, Special Publication No. 34. Hydrographic Society
Stewart RR, Huddleston PD, Kan TK (1984) Seismic versus sonic velocities: a vertical seismic profiling study. Geophysics 49:1153–1168. https://doi.org/10.1190/1.1441745
Stoll RD (1977) Acoustic waves in ocean sediments. Geophysics 42:715–725. https://doi.org/10.1190/1.1440741
Stoll RD (1989) Sediment acoustics
Strick E (1971) An explanation of observed time discrepancies between continuous and conventional well velocity surveys. Geophysics 36:285–295. https://doi.org/10.1190/1.1440169
Thomas D (1978) Seismic applications of sonic logs. The Log Analyst 19. Document ID: SPWLA-1978-vXIXn1a3
Urmos J, Wilkens RH (1993) In situ velocities in pelagic carbonates: new insights from Ocean Drilling Program Leg 130, Ontong Java Plateau. J Geophys Res 98:7903–7920. https://doi.org/10.1029/93JB00013
Ward R, Hewitt M (1977) Monofrequency borehole traveltime survey. Geophysics 42:1137–1145. https://doi.org/10.1190/1.1440779
Weill P, Mouazé D, Tessier B (2013) Internal architecture and evolution of bioclastic beach ridges in a megatidal chenier plain: field data and wave flume experiment. Sedimentology 60:1213–1230. https://doi.org/10.1111/sed.12027
Wilson J (1998) Global Temperature-Salinity Profile Programme (GTSPP)—overview and future. Intergovernmental Oceanographic Commission Technical Series. UNESCO, Paris, p 49
Winkler KW (1986) Estimates of velocity dispersion between seismic and ultrasonic frequencies. Geophysics 51:183–189. https://doi.org/10.1190/1.1442031
Wright V (1992) A revised classification of limestones. Sediment Geol 76:177–185. https://doi.org/10.1016/0037-0738(92)90082-3
Zachos J, Kroon D, Blum P, Bowles J, Gaillot P, Hasegawa T, Hathorne E (2004) Proceedings of the Ocean Drilling Program, Initial Reports, Volume 208. College Station, TX (Ocean Drilling Program). https://doi.org/10.2973/odp.proc.ir.208.2004
Acknowledgements
We are grateful to Kelvin S. Rodolfo and Joanne Whittaker for proof reading the article, and to Katharina Hochmuth for the constructive and helpful comments. We thank the reviewers for their constructive comments and suggestions. This research did not receive any specific grant from funding agencies in the public, commercial, or not-for-profit sectors. I.S. was supported under Australian Research Council’s Special Research Initiative for Antarctic Gateway Partnership (Project ID SR140300001).
Author information
Authors and Affiliations
Corresponding author
Additional information
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Electronic supplementary material
Below is the link to the electronic supplementary material.
Rights and permissions
About this article
Cite this article
Sauermilch, I., Mateo, Z.R.P. & Boaga, J. A comparative analysis of time–depth relationships derived from scientific ocean drilling expeditions. Mar Geophys Res 40, 635–641 (2019). https://doi.org/10.1007/s11001-019-09393-7
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11001-019-09393-7