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Summer SchoolGeosciences
Geology
Lecture 6 Igneous Rocks
Igneous Rocks
• Ignis is the Latin word for fire
• Igneous rocks are those formed by the consolidation, or crystallization, of magmas resulting in a mass of interlocking crystalline units or super-cooled glass
Igneous Rocks
• Magma is defined as a molten fluid, which is formed within the Earth’s crust or mantle. Magma is comprised of a complex of molten silicates with water and gasses in solution
Igneous Rocks
Classification
Igneous rocks are classified according to their:
• Rock chemistry
• Size of crystals forming the rock
Igneous RocksRock Chemistry
• Silica (chemically SiO2) is the dominant constituent in virtually all igneous rocks. Therefore classification is on the basis of silica variation:
• Ultrabasic <45% silica
• Basic 45 – 55% silica
• Intermediate 55 – 65% silica
• Acidic 65-80% silica
Igneous Rocks
Crystal Size
• If the majority of crystals have average dimensions of:
• >/= 5mm then the rocks are coarse-grained
• 1 – 5 mm rocks are medium-grained
• </= 1mm rocks are fine-grained (includes non-crystalline/glassy rocks)
Fine-grained
Obsidian
Medium-grained Granite
Coarse-grained pegmatite Granite
Igneous Rocks
• Many Igneous Rocks are PORPHYRITIC, i.e. they contain some crystals (Phenocrysts) which are much larger than the bulk of the rock. When classifying these rocks ignore the phenocrysts.
Igneous Rocks
Igneous Rocks may be of two types:
• Extrusive – those formed at the Earth’s surface
• Intrusive – those formed within the Earth’s crust
Igneous Rocks
Grain Size and rate of cooling
• Lavas tend to be fine-grained
• Hypabyssal rocks tend to be medium-grained
• Plutonic rocks tend to be course-grained
Igneous Rocks
Extrusive Rocks include:
• Lavas – which are formed from the consolidation of erupted magma
• Pyroclastic rocks – fragmented material and welded rocks produced by explosive igneous activity
• Hyaloclastites – rocks formed by the interaction of lava and water, e.g. sea or lakes
Igneous RocksIntrusive Rocks are divided into:• Hypabyssal rocks – formed from
relatively small bodies of magma, occurring along planes of weakness or fractures at comparatively shallow depths within the Earth’s crust
• Plutonic Rocks – formed from large intrusions, sometimes with areas of 1000s of kms and huge volumes of magma emplaced at considerable depth within the Earth’s crust
Igneous Rocks
• The centre of a lava may be medium-grained because it has taken longer to cool than the surface
• So the crystalline form of an igneous rock is controlled mainly by its rate of cooling
Igneous Rocks• Where magma is intruded deep within
the Earth’s crust, SLOW cooling - formation of COARSE-grained rock
• Where magmas are intruded into the Earth’s crust at shallow levels, MODERATE rates of cooling form MEDIUM-grained rock
• Where magmas are extruded onto the Earth’s surface, or into water, RAPID cooling results in FINE-grained rock
Igneous Rocks
• Using the classification diagram enables rock names to be assigned on the basis of % SiO2 and grain size
• There are no sharp boundaries between rocks of different chemistry, e.g. granites grade into syenites without a break
Igneous Rocks• The chemistry of an Igneous Rock is reflected
in its mineralogy
• Acid rocks contain ‘free’ silica – not combined with other oxides – and occurs as the mineral Quartz
• Basic rocks are relatively poor in silica, and no quartz is present, they have high content of Iron, Magnesium and Calcium oxides
Igneous RocksOther important igneous terms:
• Colour Index (CI) depends on the proportion of dark (Mafic or ferro-magnesian) minerals present
• Texture – the shapes of individual mineral grains and the relationship between them
Igneous Rocks
• Texture Terms:
• Holocrystalline – the rock is entirely crystalline
• Vitreous – containing abundant glass
Igneous Rocks
• Euhedral – grains showing perfect or near perfect crystal form
• Anhedral – showing no crystal form
• Sub-hedral – with a recognisable but imperfect crystal form
• Porphyritic – with large phenocrysts
• Equigranular – grains of approximately equal size
Igneous Rocks• Vesicular – has
cavities formerly occupied by gas bubbles
• Amygdaloidal – has cavities infilled with secondary mineral
• Xenolithic – has fragment of a foreign rock type
Igneous Rocks
Order of crystallization – the order in which the crystals in an igneous rock grew e.g. in porphyritic rock, the phenocrysts grew first and were subsequently encased in the later crystallizing groundmass
Igneous Rocks
Reading
• Press and Siever Ch. 14
• Thompson and Turk chapter on igneous rocks