GLORIA

GEOMAR Library Ocean Research Information Access

Your email was sent successfully. Check your inbox.

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

Proceed reservation?

Export
Filter
  • Fedo, Christopher M.  (2)
Material
Person/Organisation
Language
Years
  • 1
    Online Resource
    Online Resource
    Canadian Science Publishing ; 2023
    In:  Canadian Journal of Earth Sciences Vol. 60, No. 7 ( 2023-07-01), p. 839-864
    In: Canadian Journal of Earth Sciences, Canadian Science Publishing, Vol. 60, No. 7 ( 2023-07-01), p. 839-864
    Abstract: Chemical weathering indices (one-dimensional/1D index values) and accompanying ternary plots (two-dimensional/2D compositional space) facilitate quantitative comparison of whole-rock and mineral major-element data, and empirical chemical trends with predicted weathering vectors. However, data analysis in ternary plots is restricted by poles grouping elements that are hosted in different minerals or that are influenced selectively by later alteration (e.g., diagenesis/metasomatism). Tetrahedral plots (three-dimensional/3D compositional space) offer enhanced analytical utility of major-element data by shifting elements across four poles and (or) incorporating additional proxy elements. Tetrahedral space can better reveal combined effects on major-element compositions from independent mineralogical controls and post-depositional alteration via curvilinear trends that are otherwise simplified and linear in ternary space. This study focuses on mafic-rock weathering and first reviews applications and limitations of the 1D mafic index of alteration (MIA) and index of lateritization/bauxitization (IOL/IOB) that integrate into molar Al 2 O 3 –CaO * –Na 2 O–K 2 O–(FeO (T) /Fe 2 O 3(T) )–MgO and SiO 2 –Al 2 O 3 –Fe 2 O 3(T) ternary compositional space, respectively. Analysis in tetrahedral space is then demonstrated with Phanerozoic weathering profile and Precambrian paleosol data in two plots of the molar Al 2 O 3 –CaO * –Na 2 O–K 2 O–(FeO (T) /Fe 2 O 3(T) )–MgO system (A–CN–K–FM and AF–CN–K–M plots) and one plot of the molar Al 2 O 3 –CaO * –Na 2 O–K 2 O–(FeO (T) /Fe 2 O 3(T) )–MgO–SiO 2 system (A–L–F–S plot). Common chemical weathering indices are integrated into these 3D tetrahedral spaces or onto some of their 2D ternary faces. However, the tetrahedral compositional space is a key to (1) assessing integrative effects from labile element loss while accounting for the variable, redox-dependent behaviour of Fe, (2) better exposing, and correcting for, overprinting effects of diagenesis/metasomatism, and (3) tracking Si loss across all stages of chemical weathering.
    Type of Medium: Online Resource
    ISSN: 0008-4077 , 1480-3313
    Language: English
    Publisher: Canadian Science Publishing
    Publication Date: 2023
    detail.hit.zdb_id: 417294-2
    detail.hit.zdb_id: 1491201-6
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Online Resource
    Online Resource
    Canadian Science Publishing ; 2023
    In:  Canadian Journal of Earth Sciences Vol. 60, No. 7 ( 2023-07-01), p. 818-838
    In: Canadian Journal of Earth Sciences, Canadian Science Publishing, Vol. 60, No. 7 ( 2023-07-01), p. 818-838
    Abstract: Quantitatively determining the amount of chemical weathering within sedimentary rocks (and weathering profiles) took a major step forward with the creation of the chemical index of alteration (CIA) 40 years ago. The CIA relates the proportion of immobile aluminum to the mobile cations of calcium, sodium, and potassium and is grounded in empirical and modeled geochemical data for mineral reactions that occur during hydrolysis. However, the CIA should be applied cautiously because it is a one-dimensional value that in the most complex situations, as with clastic sedimentary rocks, homogenizes the compositional inputs of source, weathering, sorting, and diagenesis. Subsequently developed two-dimensional (2D) ternary diagrams (Al 2 O 3 –CaO * +Na 2 O–K 2 O; Al 2 O 3 –CaO * +Na 2 O+K 2 O–FeO+MgO) permitted the capacity to explore mineralogical-geochemical pathways in data sets that may separate those inputs, but interpreting the ternary diagrams may be complicated because they differentiate and group certain elements. Here we develop a three-dimensional tetrahedral diagram (Al 2 O 3 –CaO * +Na 2 O–K 2 O–FeO+MgO, A–CN–K–FM) that incorporates the same critical elements and permits the simultaneous assessment of felsic and mafic rocks and minerals on the same diagram while retaining the ability to separate plagioclase from alkali feldspar and monitor post-depositional potassium changes. Using the tetrahedral plot, we show that both the CIA value and positions on the 2D ternary diagrams can generate potentially misleading interpretations without properly budgeting the ferromagnesian components in parallel. We first show how the tetrahedron works, then use it with numerous previously published examples to identify how the competing mafic and felsic inputs shape the composition of source rocks, weathering profiles, actively transporting sediment, paleosols, and sedimentary rocks in sedimentary petrogenesis.
    Type of Medium: Online Resource
    ISSN: 0008-4077 , 1480-3313
    Language: English
    Publisher: Canadian Science Publishing
    Publication Date: 2023
    detail.hit.zdb_id: 417294-2
    detail.hit.zdb_id: 1491201-6
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...