THE DISTRIBUTION OF IGNEOUS ROCKS IN SPACE AND TIME CONSANGUINITY-The term consanguinity (Iddings) is used to indicate the fact that certain groups of igneous rocks, the members of which are associated in space and time, possess a community of character or family likeness which is expressed in their chemical, mineralogical, textural, and geological features. While in chemical composition consanguineous series or suites may range from acid to ultrabasic types, some mineral and chemical characters are constant, i.e. are common to practically all members; while other characters are serial, that is to say, they show regular variation throughout the series. Thus, in some suites, a constant character is oversaturation with silica, which causes free silica to appear in quite basic members. A serial character may be afforded by the regular variation of the alkalis, or of ferrous iron oxide and magnesia throughout the suite. Some series may be characterised throughout by a peculiar mineralogical feature, such as the occurrence of anorthoclase, as in certain Norwegian, East Mrican, and Antarctic suites. Consanguinity in an igneous series leads to the hypothesis that the assemblage has been derived by some process of differentiation from a common initial magma, from a number of closely related magmas.

1. CONSANGUINITY-The term consanguinity (Iddings) is used to indicate the fact that certain groups of
igneous rocks, the members of which are associated in space and time, possess a community of character or family
likeness which is expressed in their chemical, mineralogical, textural, and geological features. While in chemical
composition consanguineous series or suites may range from acid to ultrabasic types, some mineral and chemical
characters are constant, i.e. are common to practically all members; while other characters are serial, that is to
say, they show regular variation throughout the series. Thus, in some suites, a constant character is oversaturation
with silica, which causes free silica to appear in quite basic members. A serial character may be afforded by the
regular variation of the alkalis, or of ferrous iron oxide and magnesia throughout the suite. Some series may be
characterised throughout by a peculiar mineralogical feature, such as the occurrence of anorthoclase, as in certain
Norwegian, East Mrican, and Antarctic suites. Consanguinity in an igneous series leads to the hypothesis that the
assemblage has been derived by some process of differentiation from a common initial magma, from a number
of closely related magmas.
THB DIAGRAMMATIC REPRESENTATION OF IGNEOUS ROCK SERIES
The chemical and mineral relationships obtaining in a consanguineous series can be exhibited by suitable graphs
and may thus be rendered in forms which permit rapid visualisation of their characters. Diagrams of this kind are
called Variation·diagrams. The diagram which is most frequently used is one in which silica is plotted against
the other oxides in such a way that an analysis is represented by a series of points on a vertical line. By joining
up the points for each oxide in a series of analyses, curves are obtained which show graphically the variation of
each constituent with regard to silica. As the amount of silica constitutes a rough index of the stage of
differentiation a rock has reached, the curves collectively present a picture of the course of differentiation which
has produced the rock series under examination, as well as a succinct statement of its chemical characters.
Fig 1 – Silica variation diagram of Granite – Diorite series
Above Fig. illustrates a typical variation diagram, obtained by plotting analyses 2, 3, 4. and 5 in following Table
(A) and 2 in Table (B). The chemical composition of rocks dealt with in this section is illustrated by the selected
analyses given in Table
GL-Jan-2019 Igneous Petrology
Q U A R T Z – E C I E S Nikhil V. Sherekar
THE DISTRIBUTION OF IGNEOUS ROCKS IN SPACE AND TIME

2. Table (A)
Table (B)
Together these analyses represent a very common type of igneous rock series which ranges from granite to gabbro
through the intermediate stages of tonalite, quartz-diorite, and diorite. The curves are fairly regular and require
very little smoothing, indicating that the analyses plotted have real serial relations. The crosses indicate the points
for the analysis of quartz-gabbro (Table B, I). The aberrant position of these points shows that this rock is alien
to the series; and if included it would seriously disturb the regularity of the curves. Nepheline-syenite the analysis
of which is represented by circles, is clearly an even more discordant rock in this series than quartz-gabbro.
The curves for Al2O3 Cao, FeO, and MgO, all bend downwards to the right of the diagram, indicating a decrease
in these constituents as the acid end of the series is approached. These constituents are said to vary
sympathetically, the soda and potash curves, however, bend upward to the right. indicating an increase in these
constituents in the acid members of the series. They vary sympathetically with each other, but are in antipathetic
relation to Al2O3, CaO, FeO, and MgO.
It has been emphasised that variation in an igneous rock series takes place mainly in respect to the relative
proportions of the felsic and mafic groups of minerals. The silica percentage provides a rough index of this
variation in many cases, but it completely fails in some series, especially those of alkali-rich rocks. The proportion
of salic minerals, calculated from the norm, gives, on the whole, a much better index of variation. A variation-

3. diagram of the average granite-gabbro series, with the percentage of Salic minerals substituted for the silica
percentage is given in Fig.2. The curves follow much the same courses as in Fig.1, but are more regular, although
the improvement is not so apparent in this series as in many others.
In this diagram is also
shown a curve of the silica
number, which represents
the excess or defect of silica
in molecular values, in
respect to the amount which
is required just to saturate
the rock. It is obtained from
the calculation of the norm.
Free quartz computed in
molecules gives the excess
silica, while deficits are
calculated from the
amounts of olivine and
feldspathoids in the norm.
In the series illustrated by
Fig (2), only the gabbro
gives a deficit of silica. The
curve cuts the base-line, i.e.
the silica number is zero, at
the point representing 65
per cent. of felsic minerals.
A perpendicular erected at
this point may be called the
saturation line. The points
at which it cuts the curves
gives the approximate
composition of the just-
saturated rock of the series
under consideration, which
may be called the
saturation composition.
The position of the
saturation line, and the
saturation composition,
vary in different series (Figs. 45, 46), and are thus of diagnostic value. For a discussion of other types of variation
diagram the works of Harker and Holmes cited above should be consulted.
KINDREDS OF IGNEOUS ROCKS - Groups, series, or suites of igneous rocks which show
consanguineous chemical and mineral characters, and which appear to be genetically related, may be called
kindreds. Several terms have been used in closely similar senses, as series, suite, tribe, clan, branch, stem (German
stamm). The relationship implied by consanguinity may be of different degrees of closeness. The term kindred
may be used for the widest kind of grouping in which the consanguinity between the rocks is of the most tenuous
kind. Within kindred may be found tribes, the rocks of which show a closer relationship; and within tribes, clans,
with a very high degree of consanguinity. Kindreds, tribes, and clans, cut across formal classifications; and
certain abundant rock types, such as basalt, andesite, and granite, may recur in several different groupings.
Although it may be composed of a wide diversity of rock types, kindred are marked first of all by a certain
community of chemical and mineral characters, which may be exhibited in constant or serial relations. It may be
further characterised by the different bulk-development of its component rock types. Thus, in certain kindreds
andesites are the most abundant rock types, and basalt is a subordinate member i whilst in others, basalts
predominate greatly over andesites. The degree of differentiation is another factor whereby kindreds may be
distinguished. Some kindreds consist of huge masses of uniform rocks (e.g. the basalt floods) i others contain a
great diversity of types within a small compass. Furthermore, there are differences among kindreds in regard to
the relative development of plutonic, hypabyssal, and volcanic facies, at least in the accessible crust. This may,
of course, be due to accidents of erosion and exposure, but it is believed that there are also intrinsic differences
in this respect. Finally, kindreds are distinguishable by their extension in space and time (petrographic provinces
Fig 2.-Variation diagram of the Granite – Diorite Series

4. and periods) and by their varying relations to geotectonic processes. These topics will be dealt with in later
sections.
A very wide and vague, but nevertheless valid, grouping of igneous rocks, is that into alkalic and calcic (=
subalkalic, calc-alkalic), which has been much exploited in the past. It is probable that both terms cover several
distinct kindreds, and that some kindreds pass over the gradational boundary between the two groups. The terms
alkalic and calcic, nevertheless express a real tendency in igneous rocks for the separation of two broadly-
contrasted assemblages, which have different chemical, mineral, geographical, and geotectonic relations. The
mineralogical contrast may be expressed as below
Alkalic Calcic
Alkali-felspar abundant in the felsic and intermediate
rock types. And even in some mafic types.
Alkali-felspar not common except in the more silicic
rock types.
Soda-lime felspars not common except in the more
mafic types.
Soda-lime felspars abundant
throughout the range.
Felspathoids often occur. Felspathoids absent.
Quartz appears only in the more silicic rock types. Quartz occurs throughout most of the range of types,
either crystallised or occult.
Pyroxenes and amphiboles of alkali· rich varieties.
Rhombic pyroxene absent.
Ordinary augite, hornblende, and rhombic pyroxenes
present.
Micas and garnets common. Micas not common except in the more silicic rock
types. Garnets very rare.
Chemically, alkalic rocks are characterised by high percentages of alkalis in relation to silica and alumina. In
calcic rocks the ratio of alkali to silica and alumina is not so high, and constituents such as lime and the ferro-
magnesian oxides are relatively more abundant. In alkalic kindreds saturation occurs at a relatively high silica
percentage and felsic/mafic ratio; whereas in calcic kindreds the saturation composition falls at a low silica
percentage, and a comparatively small felsic/mafic ratio
PETROGRAHIC PROVINCS AND PERIODS – Province – Area Period - Time
A petrographic province is the geographical extension of a kindred, and a petrographic period is likewise its
extension in time_ The first of these terms was proposed by J. W. Judd in the following words: There are distinct
petrographical provinces within which the rocks erupted during any particular geological period present certain
well-marked peculiarities in mineralogical composition and microscopical structure, serving at once to distinguish
them from the rocks belonging to the same general group, which were simultaneously erupted in other
petrographical provinces.
A. Harker's definition is that a petrographic province is a more or less clearly defined tract within which the
igneous rocks belonging to a given period of igneous activity, present a certain community of petrographical
character traceable throughout all their diversity, or at least obscured only in some of the more extreme members
of the assemblage. In both these definitions the phrase italicised insists on a time limitation. Many objections to
the idea of petrographical provinces have been based on the mistaken view that the term applied to all the igneous
rocks within a given region regardless of their ages.
The boundaries of petrographically provinces and periods are vague and ill-defined because the true spatial and
temporal associations of a kindred are with a certain geological environment. Hence the modern tendency is to
place much more emphasis on the nature of the kindred itself, and on its connection with a definite tectonic
process, than on its mere geographical extension. For this reason, the geographical names which have been applied
alike to petrographic provinces and to kindreds, such as Atlantic for the alkalic kindreds, Pacific for the calc-
alkalic kindreds, and the later terms, such as Arctic and Mediterranean, are to be deprecated as useless and
misleading. It is nevertheless true that, for igneous rocks erupted within a given period of magmatic activity, large
areas of the earth's surface can be mapped out into more or less definite provinces in which different kindreds
hold away. The continued use of the term petrographic province it therefore justified. Similarly. The term
petrographic period may be used to indicate that petrographic provinces have a more or less definite extension in
time as well as in space.
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