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Interpretation of Whole-rock Geochemical Data in Igneous Geochemistry: Introducing Geochemical Data Toolkit (GCDkit)

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Geochemical Data Toolkit (GCDkit) is a program for handling and recalculation of geochemical data from igneous and metamorphic rocks. It is built using the Windows version of R, which provides a flexible and comprehensive language and environment for data analysis and graphics. GCDkit was designed to eliminate routine and tedious operations involving large collections of whole-rock data and, at the same time, provide access to the wealth of statistical functions built into R. Data management tools include import and export of data files in a number of formats, data editing, searching, grouping and generation of subsets. Included are a variety of calculation and normative schemes, for instance CIPW and Mesonorm, as are the common geochemical graphs (e.g. binary and ternary graphs, Harker plots, spider plots, and several dozens of classification and geotectonic discrimination diagrams). The graphical output is publication ready but can be further retouched if required. The system can be further expanded by means of plug-in modules that provide specialist applications. GCDkit is available as Free Software under the terms of the Free Software Foundation's GNU General Public License and can be downloaded from http://www.gcdkit.org. The product is actively maintained and updated to provide additional functionality; Unix/Linux and Mac OS versions are being developed.
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TECHNICAL NOTE
Interpretation of Whole-rock Geochemical
Data in Igneous Geochemistry: Introducing
Geochemical Data Toolkit (GCDkit)
VOJTE
ˇCH JANOUS
ˇEK
1,2
*, C. M. FARROW
3
AND
VOJTE
ˇCH ERBAN
1
1
CZECH GEOLOGICAL SURVEY, KLA
´ROV 3/131, 118 21 PRAGUE 1, CZECH REPUBLIC
2
INSTITUTE OF PETROLOGY AND STRUCTURAL GEOLOGY, CHARLES UNIVERSITY, ALBERTOV 6,
128 43 PRAGUE 2, CZECH REPUBLIC
3
UNIVERSITY OF GLASGOW COMPUTING SERVICE, GLASGOW G12 8QQ, UK
RECEIVED NOVEMBER 3, 2004; ACCEPTED FEBRUARY 16, 2006
ADVANCE ACCESS PUBLICATION MARCH 22, 2006
Geochemical Data Toolkit (GCDkit) is a program for handling
and recalculation of geochemical data from igneous and metamorphic
rocks. It is built using the Windows version of R, which provides
a flexible and comprehensive language and environment for data
analysis and graphics. GCDkit was designed to eliminate routine
and tedious operations involving large collections of whole-rock data
and, at the same time, provide access to the wealth of statistical
functions built into R. Data management tools include import and
export of data files in a number of formats, data editing, searching,
grouping and generation of subsets. Included are a variety of calcu-
lation and normative schemes, for instance CIPW and Mesonorm,
as are the common geochemical graphs (e.g. binary and ternary
graphs, Harker plots, spider plots, and several dozens of classifica-
tion and geotectonic discrimination diagrams). The graphical output
is publication ready but can be further retouched if required. The
system can be further expanded by means of plug-in modules that
provide specialist applications. GCDkit is available as Free
Software under the terms of the Free Software Foundation’s GNU
General Public License and can be downloaded from http://www.
gla.ac.uk/gcdkit. The product is actively maintained and updated to
provide additional functionality; Unix/Linux and Mac OS versions
are being developed.
KEY WORDS: igneous rocks; geochemistry; norms; graphs; software; MS
Windows; R language
INTRODUCTION
The challenge: geochemical recalculations
and plotting
The need to quantify aspects of the world in which we live
is inherent in contemporary scientific thinking. Such an
approach leads inevitably to a flood of numerical
data, which have to be analysed by an appropriate soft-
ware tool.
The interpretation of whole-rock geochemical data is
not different, as it requires complex and time-consuming
calculations, which on PC compatible computers are
mainly performed using dedicated, stand-alone programs
(e.g. NewPet—Clarke et al., 1994; IgPet—Carr, 1995;
MinPet—Richard, 1995; PetroGraph—Petrelli et al., 2005).
An alternative preferred by many researchers are spread-
sheets, sometimes aided by special macros (Sidder, 1994;
Su et al., 2003). Most of these otherwise useful programs
are, however, not well suited to management and inter-
pretation of larger datasets. In addition, the usability
of many of these tools is hindered by the fact that it
is often difficult to determine exactly which algorithm
has been employed, because documentation is not
detailed enough and it is not a common practice to
make the source code available. Even if it is, any
modifications or additions to the original program can
*Corresponding author. Telephone þ420 251085308. Fax: þ420
251818748. E-mail: janousek@cgu.cz
The Author 2006. Published by Oxford University Press. All
rights reserved. For Permissions, please e-mail: journals.permissions@
oxfordjournals.org
JOURNAL OF PETROLOGY VOLUME 47 NUMBER 6 PAGES 1255–1259 2006 doi:10.1093/petrology/egl013
be tedious, or impossible for legal reasons. Concerning
spreadsheets, they have low efficiency for repeated
tasks, poor quality of graphic output, as well as
limited protection of the primary data. For more com-
plicated calculations the worksheet soon becomes too
complex and prone to errors.
The solution: Geochemical Data
Toolkit (GCDkit)
To address the major drawbacks of the existing geochem-
ical software, we have developed a new package called
Geochemical Data Toolkit for R (GCDkit). GCDkit is a program
for management and recalculation of whole-rock
geochemical data for igneous and metamorphic rocks.
It is built using the open-source (freeware) R language,
version for Windows, which in itself provides a flexible
and comprehensive environment for efficient data pro-
cessing, visualization and statistical analysis (Ihaka &
Gentleman, 1996; Grunsky, 2002; R Development
Core Team, 2005).
GCDkit provides:
(1) a graphical user interface aiding the user with pull-
down menus and dialogue boxes (Fig. 1);
(2) user-friendly front-end to the powerful statistical and
graphical functions of R;
(3) core routines for effortless import, modification,
searching, subsetting, classification and output of the
geochemical data;
(4) calculation and plotting tools designed specifically for
igneous geochemists;
(5) flexible and high-level graphical functions with an
output into widely used graphical formats;
(6) no licensing problems, as it is distributed free via the
WWW.
PROGRAM DESCRIPTION
Data management
The main area of application for GCDkit is the interpreta-
tion of larger datasets. Accordingly, great emphasis has
Fig. 1. Typical screen display of R with embedded GCDkit.
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JOURNAL OF PETROLOGY VOLUME 47 NUMBER 6 JUNE 2006
been put on data management tools (loading and saving
data files, data editing, together with searching and
generation of subsets).
GCDkit can read plain text files, including the variants
represented by the NewPet (*.ROC) and PetroGraph
(*.PEG) files as well as the outputs from WWW-based
databases such as GEOROC (http://georoc.mpch-mainz.
gwdg.de/georoc) and PETDB (http://www.petdb.org).
Data can be imported from Microsoft Excel (*.XLS),
Access (*.MDB), or dBase (*.DBF) formats, the latter
being the native format for IgPet (Carr, 1995) or MinPet
(Richard, 1995) packages. As an alternative, the data can
be pasted, via the clipboard, from any Windows-based
software, including popular spreadsheets. In any case
the data are freeform, which means that the columns
can be given in an arbitrary order and missing values
are allowed.
Grouping of data is a key part of data management,
controlling the output of calculations and the graphical
routines. Analyses may be grouped on the basis of various
criteria including sample attributes, so-called labels
(locality, rock type, etc.), numerical variable, cluster
analysis or selected classification diagram (e.g. total
alkali–silica). For greatest flexibility queries may be logic-
ally combined, allowing, for example, selection based on
rock type and contents of particular elements. Interactive
selection from classification diagrams is also supported.
Calculations
New variables can be calculated by mathematical expres-
sions including constants, brackets, arithmetic operators
and the whole spectrum of R functions. Statistical func-
tions include descriptive statistics, box-and-whiskers and
correlation plots or multivariate methods. Also imple-
mented are a variety of calculation schemes used in igne-
ous geochemistry, for instance CIPW norm, Catanorm,
Niggli’s cationic values, multicationic parameters of
De La Roche et al. (1980) and Debon & Le Fort (1983),
and improved Mesonorm for granitoid rocks (Mielke &
Winkler, 1979). Given major-element analyses of a rock
and its main mineral constituents, the best approximation
of the modal composition, using either unconstrained or
constrained least-squares methods (Albare
`de, 1995), may
be calculated.
The results of all calculations can be appended to the
current dataset for further processing (e.g. CIPW-
normative albite, quartz and orthoclase to be plotted on
a Ab–Qz–Or ternary diagram) or copied to a clipboard,
saved or exported to HTML, DBF, XLS, MDB or text files.
Plotting
The main strength of GCDkit is arguably the wealth of
built-in publication-quality plots that can be exported
into a number of data formats (including PostScript,
WMF, JPG, PNG and BMP). The available graphs
involve user-defined binary, ternary and multiple binary
diagrams (such as Harker plots) as well as a wide palette
of classification and geotectonic discrimination diagrams.
Three variables can be displayed in pseudo three-
dimensional plots, or on binary diagrams in which the
size and colour of the plotted symbols correspond to the
third variable (Fig. 2a).
All plots are publication ready but most can be
customized with the included plot editing facilities. The
system permits zooming and scaling of the diagrams,
editing of the text, font, size and colour of the titles and
axis labels, and of the colour, size and symbol for the data
points, together with colour, type and width of the lines.
Moreover, there is a function for interactive labelling of
individual analyses (typically by sample names but other
labels can be specified). The graph templates can be used
also as a basis for classification. Put simply, the classifica-
tion algorithm looks for the name of the polygon within
the diagram, into which the rock analysis falls according
to its xycoordinates.
GCDkit offers normalization of trace-element data by
any chosen standard and the ability to generate normal-
ized multielement diagrams, otherwise called ‘spider
plots’. One special feature are the ‘spider boxplots’, in
which no individual patterns are drawn. Instead, the
statistical distribution of each element is portrayed by a
box-and-whiskers plot of normalized concentrations
(Fig. 2b). The standard compositions used for normaliza-
tion can be readily edited and new schemes added. For
visualization of larger datasets there are contour and
frequency plots (Fig. 2c).
Expandability
The open architecture and simplicity mean that users will
readily be able to further enhance the capabilities of the
system, by modifying existing functions or creating new
ones. The system incorporates a plug-in mechanism
whereby new calculation or plotting code is automatically
loaded and made accessible through the menu system.
Included with the current version are plug-in modules
to calculate saturation temperatures of accessory minerals
( Janous
ˇek, 2006) as well as for interpretation of Sr–Nd
isotopic data (Fig. 2d).
CONCLUDING REMARKS
GCDkit will run on any IBM PC compatible computer
with Windows 98/ME/2000/NT/XP (but latest versions
are strongly recommended). The program with cor-
responding documentation is available free of charge at
http://www.gla.ac.uk/gcdkit and is easy to install.
1257
JANOUS
ˇEK et al. TECHNICAL NOTE
Our mission is to develop and release a platform-
independent system, for Windows, Unix/Linux and
Macintosh (System X). In the shorter-term perspective,
new plug-ins for direct and inverse modelling of major
petrogenetic processes in igneous geochemistry are under
development.
The whole system, which is modular and straight-
forward to modify, provides a practical solution to
the needs of petrologists and geochemists. If current
modules do not meet requirements, or new techniques
evolve, it is hoped that the open source availability of
the code will encourage its onward development by
users. In this context any feedback (bug reports,
suggestions for further development, and pieces of
contributed code or even ready plug-ins) would be
highly appreciated.
Fig. 2. Examples of diagrams generated by GCDkit. (a) SiO
2
–MgO plot for granitoids of the Variscan Central Bohemian Pluton, Czech Republic,
with size and grey shade of the plotting symbols corresponding to the K
2
O contents of individual samples. The data are from Janous
ˇek et al. (2000,
and unpublished). (b) Average upper crust normalized (Taylor & McLennan, 1985) ‘spider boxplots’ for felsic Variscan granulites from the
Moldanubian Unit, Bohemian Massif ( Janous
ˇek et al., 2004). (See text for explanation.) (c) SiO
2
–K
2
O plot with the discrimination boundaries
between the tholeiitic, calc-alkaline, high-K calc-alkaline and shoshonitic rocks of Peccerillo & Taylor (1976). Contoured grey fields are for all
available analyses from Moldanubian granulites and data points are for the Lis
ˇov Massif, Southern Bohemia ( Janous
ˇek et al., 2006). (d) Two-stage
Nd isotope development diagram for felsic Moldanubian granulites. DM, Depleted Mantle evolution lines after Goldstein et al. (1984) and Liew &
Hofmann (1988); CHUR, Chondritic Uniform Reservoir. The extra tick marks on axes show two-stage Nd model ages (x-axis) and initial
e
Nd
values ( y-axis).
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JOURNAL OF PETROLOGY VOLUME 47 NUMBER 6 JUNE 2006
ACKNOWLEDGEMENTS
We are indebted to Jakub S
ˇ
´d for much of the ternary
plotting function, the Core Team and the whole com-
munity for their sterling efforts in continuous developing
of R—GCDkit is often merely an interface to their func-
tions. Thanks are specifically due to Friedrich Leisch
(Technische Universita
¨t Wien) and Duncan Murdoch
(University of Western Ontario) for their invaluable
advice. Last but not least, we thank beta testers (in
particular Pavel Hanz
ˇl and Bernhard Humer) for their
courage and patience, and the students in Prague, Brno
and Salzburg for asking nasty questions. This paper and
the program itself has benefited from extensive testing,
detailed comments and words of encouragement of
J.-F. Moyen. Also, the reviews by R. Giere, D. Geist
and T. Barry have helped us to improve aspects of the
software. Most of the coding of GCDkit originated during
the research stay of V.J. at the Institute of Mineralogy,
University of Salzburg, in the framework of the FWF
Project 15133-GEO (to Fritz Finger). Support from the
Czech Grant Agency (Postdoctoral Grant 205/97/P113)
and the Czech Geological Survey (Internal Project 3314)
is gratefully acknowledged.
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Supplementary resources (2)

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We report here the presence of tuffs from the Neoproterozoic Bhima basin unreported hitherto. These are exposed near Hotpet, Hulkal, Kanchankavi, and Ukinal area along two different stratigraphic horizons (1) within carbonates of Shahabad Formation and (2) above shale of Hulkal Formation. Tuffs are of two types: 1. Ash fall tuff and 2. Lapilli tuff, occurring as beds, matrix of a conglomeratic unit and patchy discontinuous layers. Physically ash fall tuff is thinly bedded (2-6 cm) and light-weight, lapilli tuff is hard, compact and individual beds are not discernible in the field. Presence of petrological features like bipyramidal quartz, fiamme structures, embayed quartz grains, blue CL colours of quartz grains, volcanic layering and banding, altered glass, and stretched and elongated volcanic glasses, are clear indications of its volcanic affinity. The tuff is anomalously high in silica content ranging from 71.4-91.2wt% and have low alumina value ranging from 0.75-4.11 wt % compared with that of the normal felsic tuffs, rhyolites and high silica rhyolites. REE in the tuffs can be grouped into two types, 1. Ash fall tuff with enriched LREE and fractionated HREE, 2. Lapilli tuff with flat LREE and HREE pattern. Tuff shows high Hf, overall enrichment of large ion lithophile elements (LILE Rb, Th, K and Pb) and depletion in HFSEs (Nb, Ta, Ti, P). The tuff is probably generated from continental crust source and the depositions are episodic and have more than one eruptive pulses of volcanic activity.
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The Lisov Granulite Massif differs from neighbouring granulite bodies in the Moldanubian Zone of southern Bohemia (Czech Republic) in including a higher proportion of intermediate-mafic and orthopyroxene-bearing rocks, associated with spinel peridotites but lacking eclogites. In addition to dominantly felsic garnet granulites, other major rock types include quartz dioritic two-pyroxene granulites, tonalitic granulites and charnockites. Minor bodies of high-pressure layered gabbroic garnet granulites and spinel peridotites represent tectonically incorporated foreign elements. The protoliths of the mafic-intermediate granulites (quartz-dioritic and tonalitic) crystallized [~]360-370 Ma ago, as indicated by laser ablation inductively coupled plasma mass spectrometry U-Pb ages of abundant zircons with well-preserved magmatic zoning. Strongly metamorphically recrystallized zircons give ages of 330-340 Ma, similar to those of other Moldanubian granulites. For the overwhelming majority of the Li[s]ov granulites peak metamorphic conditions probably did not exceed 800-900{degrees}C at 4-5 kbar; the equilibration temperature of the pyroxene granulites was 670-770{degrees}C. This is in sharp contrast to conditions of adjacent contemporaneous Moldanubian granulites, which are characterized by a distinct HP-HT signature. The mafic-intermediate Li[s]ov granulites are thought to have originated during Visean metamorphic overprinting of metaluminous, medium-K calc-alkaline plutonic rocks that formed the mid-crustal root of a Late Devonian magmatic arc. The protolith resembled contemporaneous calc-alkaline intrusions in the European Variscan Belt
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A new software, PetroGraph, has been developed to visualize, elaborate, and model geochemical data for igneous petrology purposes. The software is able to plot data on several different diagrams, including a large number of classification and “petrotectonic” plots. PetroGraph gives the opportunity to handle large geochemical data sets in a single program without the need of passing from one software to the other as usually happens in petrologic data handling. Along with these basic functions, PetroGraph contains a wide choice of modeling possibilities, from major element mass balance calculations to the most common partial melting and magma evolution models based on trace element and isotopic data. Results and graphs can be exported as vector graphics in publication-quality form, or they can be copied and pasted within the most common graphics programs for further modifications. All these features make PetroGraph one of the most complete software presently available for igneous petrology research.
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The prominent felsic granulites in the southern part of the Bohemian Massif (Gföhl Unit, Moldanubian Zone), with the Variscan (∼340 Ma) high-pressure and high-temperature assemblage garnet+quartz+hypersolvus feldspar ± kyanite, correspond geochemically to slightly peraluminous, fractionated granitic rocks. Compared to the average upper crust and most granites, the U, Th and Cs concentrations are strongly depleted, probably because of the fluid and/or slight melt loss during the high-grade metamorphism (900–1050°C, 1·5–2·0 GPa). However, the rest of the trace-element contents and variation trends, such as decreasing Sr, Ba, Eu, LREE and Zr with increasing SiO 2 and Rb, can be explained by fractional crystallisation of a granitic magma. Low Zr and LREE contents yield ∼750°C zircon and monazite saturation temperatures and suggest relatively low-temperature crystallisation. The granulites contain radiogenic Sr ( ⁸⁷ Sr/ ⁸⁶ Sr 340 = 0·7106–0·7706) and unradiogenic Nd ( = − 4·2 to − 7·5), indicating derivation from an old crustal source. The whole-rock Rb–Sr isotopic system preserves the memory of an earlier, probably Ordovician, isotopic equilibrium. Contrary to previous studies, the bulk of felsic Moldanubian granulites do not appear to represent separated, syn-metamorphic Variscan HP–HT melts. Instead, they are interpreted as metamorphosed (partly anatectic) equivalents of older, probably high-level granites subducted to continental roots during the Variscan collision. Protolith formation may have occurred within an Early Palaeozoic rift setting, which is documented throughout the Variscan Zone in Europe.
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Modern geochemistry aims to provide an accurate description of geological processes, and a set of models and quantitative rules that help predict the evolution of geological systems. This work is an introduction to the mathematical methods of geochemical modeling, largely based on examples presented with full solutions. It shows how geochemical problems, dealing with mass balance, equilibrium, fractionation, dynamics, and transport in the igneous, sedimentary and oceanic environments, can be reformulated in terms of equations. Its practical approach then leads to simple but efficient methods of solution. This book should help the motivated reader to overcome the formal difficulties of geochemical modeling, and bring state-of-the-art methods within reach of advanced students in geochemistry and geophysics, as well as in physics and chemistry.
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A classification is proposed, based mainly on major element analytical data plotted in a coherent set of three simple chemical-mineralogical diagrams. The procedure follows two complementary steps at two different levels. The first is concerned with the individual sample: the sample is given a name (e.g. granite, adamellite, granodiorite) and its chemical and mineralogical characteristics are determined. The second one is more important: it aims at defining the type of magmatic association (or series) to which the studied sample or group of samples belongs. Three main types of association are distinguished: cafemic (from source-material mainly or completely mantle-derived), aluminous (mainly or completely derived by anatexis of continental crust), and alumino-cafemic (intermediate between the other two types). Subtypes are then distinguished among the cafemic and alumino-cafemic associations: calc-alkaline (or granodioritic), subalkaline (or monzonitic), alkaline (and peralkaline), tholeiitic (or gabbroic-trondhjemitic), etc. In the same way, numerous subtypes and variants are also distinguished among the aluminous associations using a set of complementary criteria such as quartz content, colour index, alkali ratio, quartz–alkalies relationships and alumina index. Although involving a new approach using partly new criteria, this classification is consistent with most of the divisions used in previous typologies. The method may also be used in the classification of the volcanic equivalents of common plutonic rocks.
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The R1R2 chemical variation diagram, which includes all of the major cations, a mineralogical network, the degree of silica saturation, and the combined changes in and ratios in igneous rocks, is proposed where:R1 and R2 are parameters calculated either from chemical analyses (oxide percentages converted to millications) or modal data.Statistical distributions of “current rock names” are given for three large geochemical files: CLAIR, PETROS and RKFNSYS. A single classification grid, applicable to both volcanic and plutonic rocks, is proposed which is consistent with basic petrology. Successive belts spread from two fields, “peridotic” and “granitic or rhyolitic”, respectively, with a poorly-defined intersection in the region of intermediate rock compositions. The radial subdivisions crossing the successive belts are consistent with igneous differentiation suites. On the grid, isovalue lines of silica contents clearly cut across the boundaries between successive natural belts, except for the calc-alkaline series. Classifications based on silica contents are thus inconsistent with the current use of nomenclature. The grid has been applied to redefine the mean chemical compositions of 46 principal igneous rock types.
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This book describes the composition of the present upper crust, and deals with possible compositions for the total crust and the inferred composition of the lower crust. The question of the uniformity of crustal composition throughout geological time is discussed. It describes the Archean crust and models for crustal evolution in Archean and Post-Archean time. The rate of growth of the crust through time is assessed, and the effects of the extraction of the crust on mantle compositions. The question of early pre-geological crusts on the Earth is discussed and comparisons are given with crusts on the Moon, Mercury, Mars, Venus and the Galilean Satellites.
Book
Modern geochemistry aims to provide an accurate description of geological processes, and a set of models and quantitative rules that help predict the evolution of geological systems. This work is an introduction to the mathematical methods of geochemical modeling, largely based on examples presented with full solutions. It shows how geochemical problems, dealing with mass balance, equilibrium, fractionation and dynamics and transport in the igneous, sedimentary and oceanic environments, can be reformulated in terms of equations. Its practical approach then leads to simple but efficient methods of solution. This book should help the motivated reader to overcome the formal difficulties of geochemical modeling, and bring state-of-the-art methods within reach of advanced students in geochemistry and geophysics, as well as in physics and chemistry.
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PETRO.CALC.PLOT is a package of macros which normalizes whole-rock oxide data to 100%, calculates the cation percentages and molecular proportions used for normative mineral calculations, computes the apices for ternary diagrams, determines sums and ratios of specific elements of petrologic interest, and plots 33 X-Y graphs and five ternary diagrams. PETRO.CALC.PLOT also may be used to create other diagrams as desired by the user. The macros run in Microsoft Excel 3.0 and 4.0 for Macintosh computers and in Microsoft Excel 3.0 and 4.0 for Windows. Macros provided in PETRO.CALC.PLOT minimize repetition and time required to recalculate and plot whole-rock oxide data for petrologic analysis.