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Lithocap Structure-controlled feeder zone Lithology-controlled ...

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Cretaceous-<br />

Paleogene<br />

Lepanto<br />

metavolcanics<br />

12-13 Ma Bagon<br />

intrusive complex<br />

Late Oligocene to mid-<br />

Miocene Apaoan<br />

volcaniclastics<br />

Slightly younger Balili<br />

volcaniclastics<br />

Qtz diorite<br />

1 km<br />

porphyry<br />

Imbanguila<br />

dacite<br />

Imbanguila<br />

pyroclastics<br />

(3.3-1.8 Ma)<br />

Qtz diorite<br />

1 km porphyry<br />

Cretaceous-<br />

Paleogene<br />

Lepanto<br />

metavolcanics<br />

12-13 Ma Bagon<br />

intrusive complex<br />

Late Oligocene to mid-<br />

Miocene Apaoan<br />

volcaniclastics<br />

Slightly younger Balili<br />

volcaniclastics<br />

porphyry<br />

(3.3-1.8 Ma)<br />

Pliocene<br />

volcanism<br />

3.3 - 1.8 Ma,<br />

multiple eruptions<br />

Imbanguila<br />

dacite<br />

Imbanguila<br />

pyroclastics<br />

(3.3-1.8 Ma)<br />

Qtz diorite<br />

1 km porphyry<br />

Cretaceous-<br />

Paleogene<br />

Lepanto<br />

metavolcanics<br />

12-13 Ma Bagon<br />

intrusive complex<br />

Bato pyroclastics<br />

(1.2 Ma)<br />

Bato dacite<br />

porphyry (1.2 Ma)<br />

Lapangan Tuff<br />

(0.19 Ma)<br />

Late Oligocene to mid-<br />

Miocene Apaoan<br />

volcaniclastics<br />

Slightly younger Balili<br />

volcaniclastics<br />

porphyry<br />

(3.3-1.8 Ma)<br />

Young<br />

cover:<br />

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