Skip navigation

Items where Author is "Pearce, T. J."

Items where Author is "Pearce, T. J."

Up a level
Export as [feed] RSS
Group by: Item Type | Uncontrolled Keywords | No Grouping
Number of items: 4.

Carboniferous

Pearce, T. J., McLean, D., Martin, J. H., Ratcliffe, K. T. and Wray, D. ORCID: 0000-0002-0799-2730 (2010) A whole-rock geochemical approach to the recognition and correlation of "marine bands". In: Ratcliffe, Kenneth T. and Zaitlin, Brian A., (eds.) Application of Modern Stratigraphic Techniques: Theory and Case Histories. SEPM Special Publication (94). SEPM (Society for Sedimentary Geology), pp. 221-238. ISBN 978-1-56576-199-5

chemostratigraphy

Pearce, T. J., McLean, D., Martin, J. H., Ratcliffe, K. T. and Wray, D. ORCID: 0000-0002-0799-2730 (2010) A whole-rock geochemical approach to the recognition and correlation of "marine bands". In: Ratcliffe, Kenneth T. and Zaitlin, Brian A., (eds.) Application of Modern Stratigraphic Techniques: Theory and Case Histories. SEPM Special Publication (94). SEPM (Society for Sedimentary Geology), pp. 221-238. ISBN 978-1-56576-199-5

marine bands

Pearce, T. J., McLean, D., Martin, J. H., Ratcliffe, K. T. and Wray, D. ORCID: 0000-0002-0799-2730 (2010) A whole-rock geochemical approach to the recognition and correlation of "marine bands". In: Ratcliffe, Kenneth T. and Zaitlin, Brian A., (eds.) Application of Modern Stratigraphic Techniques: Theory and Case Histories. SEPM Special Publication (94). SEPM (Society for Sedimentary Geology), pp. 221-238. ISBN 978-1-56576-199-5

palynology

Pearce, T. J., McLean, D., Martin, J. H., Ratcliffe, K. T. and Wray, D. ORCID: 0000-0002-0799-2730 (2010) A whole-rock geochemical approach to the recognition and correlation of "marine bands". In: Ratcliffe, Kenneth T. and Zaitlin, Brian A., (eds.) Application of Modern Stratigraphic Techniques: Theory and Case Histories. SEPM Special Publication (94). SEPM (Society for Sedimentary Geology), pp. 221-238. ISBN 978-1-56576-199-5

This list was generated on Fri Nov 22 03:52:35 2024 UTC.