VARIASI KEDALAMAN DISKONTINUITAS MOHO DI JAWA TENGAH DAN YOGYAKARTA BERDASARKAN DATA RECEIVER FUNCTION

• المؤلفون الرئيسيون: , NOOR ACHID YUNARTHA, , Dr. rer. nat. Wiwit Suryanto, M.Si
• التنسيق: Theses and Dissertations NonPeerReviewed
• منشور في: [Yogyakarta] : Universitas Gadjah Mada 2013
• الموضوعات: ETD
• الوصول للمادة أونلاين: https://repository.ugm.ac.id/123790/; http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=63905

Mohorovi�i� discontinuity or Moho is a boundary between the crust and upper mantle. This boundary has a characteristic that P wave velocity increased from 6,75 km/s up to 8 km/s. The velocity contrast between crust and mantle can be used to estimate the crustal thickness. Tectonic process is a fac...