Pemanfaatan Hasil Riset Kepingan Kerak Samudra Purba dalam Perspektif Dinamika Kerak Bumi Aktual
Keywords:
Kerak Samudra Purba, Ofiolit, Petrologi-GeokimiaSynopsis
Penelitian geologi, petrologi, geokimia kepingan kerak samudra purba yang tersebar di beberapa pulau di Indonesia mengindikasikan sebagai jejak konvergensi lempengan bumi di masa lalu. Kepingan-kepingan kerak samudra di Indonesia terbentuk dalam lingkungan tektonik yang beragam, yaitu terbentuk dalam lingkungan busur gunungapi, punggungan tengah samudra, basal kepulauan samudra dan sub-kontinen. Hasil pengukuran umur pembentukan batuan memberikan rentang waktu mulai dari Kala Jura Tengah (157 Juta Tahun Lalu) sampai umur temuda 15-9 Juta tahun lalu atau Kala Miosen Tengah-Akhir. Asal usul dan rentang umur pembentukan kepingan kerak samudra memberikan gambaran baru tatanan geologi dan tektonik terkait dengan pembentukan sumber daya energi atau migas. Secara alamiah komposisi kimia dan kandungan unsur logam ekonomis seperti nikel, krom, kobal, titanium maupun seng yang berbeda dari kerak samudra yang terbentuk dari selubung bumi. Dalam perspektif dinamika kerak bumi aktual, pemahaman dan pengetahuan dasar kerak bumi dapat dijadikan sebagai bahan dalam upaya mitigasi bencana. Pergerakan kerak bumi juga dapat membentuk sumber daya mineral dalam lingkungan kegiatan vulkanik. Kerak samudra yang merupakan alas dari dasar laut sangat strategis sifatnya bagi Indonesia sebagai negara benua maritim. Perluasan wilayah laut di luar 200 nm dalam jangka panjang akan sangat bermanfaat bagi Indonesia.
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