Hubungan Kerapatan Struktur dengan Gravitasi Residu; studi kasus di Gunung Muria, Jawa Tengah.

Fajar Rizki Widiatmoko, Ratih Hardini Kusuma Putri, Huzaely Latief Sunan

Abstract


Penggunaan metode analisis kerapatan struktur / fault fracture density
(FFD) secara masif digunakan selama satu dekade terakhir, terutama
pada studi pendahuluan panas bumi yang dapat menunjukkan prospek
wilayah waduk. Artikel ini membahas tentang korelasi nilai FFD
dengan nilai gravitasi residu yang dianggap sebagai indikasi benda
magmatik di bawahnya. Korelasi nilai FFD dengan nilai gravitasi residu
diterapkan di pegunungan Muria. Gunung Muria tergolong badan
gunungapi yang mengandung badan magmatik, juga ada gunung api
Genuk dan bukit Patiayam di sekitar Muria.

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