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TEXTURAL AND MICROANALYSIS OF IGNEOUS ROCKS: TOOLS ...

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3.5.4 Major Elements<br />

Major element compositions measured by EPMA and Ti abundances measured<br />

by LA-ICP-MS in plagioclase crystals from each Unit are reported in table 3.3<br />

and illustrated in figure 3.9.<br />

3.5.4.1 Site 1203 Unit 3<br />

I noted variations in An content apparent in backscatter electron images that<br />

correlate with zoning patterns. Unit 3 Population A crystal cores fall into two<br />

groups in terms of An content. The higher An group (An74−79) overlaps the<br />

population B cores (An78−81) (Fig. 3.9a). The cores of population B crystals<br />

extend to higher An contents (up to An81) than population A crystals. There is<br />

no obvious variation in Mg # (measured in plagioclase) between population A<br />

and B crystals or with An content.<br />

3.5.4.2 Site 1203 Unit 14<br />

The cores of population A crystals from Unit 14 also fall into two groups in<br />

terms of An content. The more An rich population A group have An77−82 cores<br />

that overlap the compositions of population B cores, and the lower An population<br />

A group have An64−76 cores. The cores of population B crystals have a higher<br />

range of An content (An81−87), but a single population B crystal with a core<br />

composition of An73−74 was observed. There is no obvious variation in Mg #<br />

(Mg/Mg+total Fe measured in plagioclase) between population A and B crystals<br />

or with An content, but a single Unit 14 crystal rim (An56) has the lowest overall<br />

Mg # (Fig. 3.9d).<br />

113

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