Seismic Structure Beneath the Molucca Sea Collision Zone from Travel Time Tomography Based on Local and Regional BMKG Networks
, Bagus Jaya Santosa 1, Andri Dian Nugraha 3,4, Supriyanto Rohadi 5, Shindy Rosalia 3,4, Zulfakriza Zulfakriza 3,4, Sungkono Sungkono 1, David P. Sahara 3,4, Faiz Muttaqy 6, Pepen Supendi 5, Mohamad Ramdhan 6, Ardianto Ardianto 7 and Haunan Afif 8Round 1
Reviewer 1 Report
The authors used lots of P and S phases from the local events to get the P wave and S wave velocity beneath the Molucca Sea Collision Zone.
The data is enough, the method has been highly used before, and the results seem confusing. Why does the slab not have the high velocity in Figure 6 and Figure 7?
Author Response
Dear Reviewer-1,
Please see the attachment file for our respond to your comments/suggestions.
Thank you
Author Response File: 
Author Response.docx
Reviewer 2 Report
Comments for author File: Comments.docx
Author Response
Dear Reviewer 2,
Please see the attachment file for our responds to your comments/suggestions.
Thank you
Author Response File: Author Response.docx
Round 2
Reviewer 2 Report
Dear Editor,
I carefully read the paper entitled “Seismic Structure Beneath the Molucca Sea Collision Zone from Travel Time Tomography Based on Local and Regional BMKG Networks” by Rachman and co-authors.
The authors addressed all the comments and, in my opinion, the critical sections now are in a good shape. For these reasons, I suggest accepting the paper in the present form.
I wish the authors good luck.
Best regards
