http://hdl.handle.net/10256/641 2025-06-02T11:59:45Z 2025-06-02T11:59:45Z Burger, H. Kuhn, T. http://hdl.handle.net/10256/731 2022-07-13T06:59:26Z 2008-05-28T00:00:00Z

Application of compositional data analysis to geochemical data of marine sediments Burger, H.; Kuhn, T. Daunis-i-Estadella, Pepus; Martín Fernández, Josep Antoni In an earlier investigation (Burger et al., 2000) five sediment cores near the Rodrigues Triple Junction in the Indian Ocean were studied applying classical statistical methods (fuzzy c-means clustering, linear mixing model, principal component analysis) for the extraction of endmembers and evaluating the spatial and temporal variation of geochemical signals. Three main factors of sedimentation were expected by the marine geologists: a volcano-genetic, a hydro-hydrothermal and an ultra-basic factor. The display of fuzzy membership values and/or factor scores versus depth provided consistent results for two factors only; the ultra-basic component could not be identified. The reason for this may be that only traditional statistical methods were applied, i.e. the untransformed components were used and the cosine-theta coefficient as similarity measure. During the last decade considerable progress in compositional data analysis was made and many case studies were published using new tools for exploratory analysis of these data. Therefore it makes sense to check if the application of suitable data transformations, reduction of the D-part simplex to two or three factors and visual interpretation of the factor scores would lead to a revision of earlier results and to answers to open questions . In this paper we follow the lines of a paper of R. Tolosana- Delgado et al. (2005) starting with a problem-oriented interpretation of the biplot scattergram, extracting compositional factors, ilr-transformation of the components and visualization of the factor scores in a spatial context: The compositional factors will be plotted versus depth (time) of the core samples in order to facilitate the identification of the expected sources of the sedimentary process. Kew words: compositional data analysis, biplot, deep sea sediments

2008-05-28T00:00:00Z Grunsky, Eric C. Kjarsgaard, Bruce A. Egozcue, Juan José Pawlowsky-Glahn, Vera Thió i Fernández de Henestrosa, Santiago http://hdl.handle.net/10256/730 2022-11-30T09:44:44Z 2008-05-28T00:00:00Z

Studies in stoichiometry with compositional data Grunsky, Eric C.; Kjarsgaard, Bruce A.; Egozcue, Juan José; Pawlowsky-Glahn, Vera; Thió i Fernández de Henestrosa, Santiago Daunis-i-Estadella, Pepus; Martín Fernández, Josep Antoni Geochemical data that is derived from the whole or partial analysis of various geologic materials represent a composition of mineralogies or solute species. Minerals are composed of structured relationships between cations and anions which, through atomic and molecular forces, keep the elements bound in specific configurations. The chemical compositions of minerals have specific relationships that are governed by these molecular controls. In the case of olivine, there is a well-defined relationship between Mn-Fe-Mg with Si. Balances between the principal elements defining olivine composition and other significant constituents in the composition (Al, Ti) have been defined, resulting in a near-linear relationship between the logarithmic relative proportion of Si versus (MgMnFe) and Mg versus (MnFe), which is typically described but poorly illustrated in the simplex. The present contribution corresponds to ongoing research, which attempts to relate stoichiometry and geochemical data using compositional geometry. We describe here the approach by which stoichiometric relationships based on mineralogical constraints can be accounted for in the space of simplicial coordinates using olivines as an example. Further examples for other mineral types (plagioclases and more complex minerals such as clays) are needed. Issues that remain to be dealt with include the reduction of a bulk chemical composition of a rock comprised of several minerals from which appropriate balances can be used to describe the composition in a realistic mineralogical framework. The overall objective of our research is to answer the question: In the cases where the mineralogy is unknown, are there suitable proxies that can be substituted? Kew words: Aitchison geometry, balances, mineral composition, oxides

2008-05-28T00:00:00Z Buccianti, Antonella Tassi, Franco Vaselli, Orlando Montegrossi, Giordano http://hdl.handle.net/10256/729 2022-07-13T06:59:26Z 2008-05-28T00:00:00Z

Statistical evidences of cyclic changes in volcanic gas chemistry composition by inverse modelling Buccianti, Antonella; Tassi, Franco; Vaselli, Orlando; Montegrossi, Giordano Daunis-i-Estadella, Pepus; Martín Fernández, Josep Antoni The identification of compositional changes in fumarolic gases of active and quiescent volcanoes is one of the most important targets in monitoring programs. From a general point of view, many systematic (often cyclic) and random processes control the chemistry of gas discharges, making difficult to produce a convincing mathematical-statistical modelling. Changes in the chemical composition of volcanic gases sampled at Vulcano Island (Aeolian Arc, Sicily, Italy) from eight different fumaroles located in the northern sector of the summit crater (La Fossa) have been analysed by considering their dependence from time in the period 2000-2007. Each intermediate chemical composition has been considered as potentially derived from the contribution of the two temporal extremes represented by the 2000 and 2007 samples, respectively, by using inverse modelling methodologies for compositional data. Data pertaining to fumaroles F5 and F27, located on the rim and in the inner part of La Fossa crater, respectively, have been used to achieve the proposed aim. The statistical approach has allowed us to highlight the presence of random and not random fluctuations, features useful to understand how the volcanic system works, opening new perspectives in sampling strategies and in the evaluation of the natural risk related to a quiescent volcano

2008-05-28T00:00:00Z Lee, Bik-wa Bacon Shone, John http://hdl.handle.net/10256/728 2022-07-13T06:59:26Z 2008-05-28T00:00:00Z

An alternative method for dating unknown tephras based on a segmented regression model Lee, Bik-wa; Bacon Shone, John Daunis-i-Estadella, Pepus; Martín Fernández, Josep Antoni In CoDaWork’05, we presented an application of discriminant function analysis (DFA) to 4 different compositional datasets and modelled the first canonical variable using a segmented regression model solely based on an observation about the scatter plots. In this paper, multiple linear regressions are applied to different datasets to confirm the validity of our proposed model. In addition to dating the unknown tephras by calibration as discussed previously, another method of mapping the unknown tephras into samples of the reference set or missing samples in between consecutive reference samples is proposed. The application of these methodologies is demonstrated with both simulated and real datasets. This new proposed methodology provides an alternative, more acceptable approach for geologists as their focus is on mapping the unknown tephra with relevant eruptive events rather than estimating the age of unknown tephra. Kew words: Tephrochronology; Segmented regression

2008-05-28T00:00:00Z