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by
  • Gazali Rachman1,2,*,
  • Bagus Jaya Santosa1 and
  • Andri Dian Nugraha3,4
  • et al.

Reviewer 1: Anonymous Reviewer 2: Anonymous

Round 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