Wireline Sonic Waveform Data

DSDP operator and logging contractor: Scripps Institution of Oceanography

Hole: 564

Leg: 82

Location: Mid-Atlantic Ridge (central N Atlantic)

Latitude: 33° 44.36' N

Longitude: 43° 46.03' W

Logging date: October 1981

Sea floor depth (drillers' mudline): 3830 mbrf

Sea floor depth (step in GR log): 3830 mbrf

Total penetration: 365 mbsf

Total core recovered: 34.75 m (43 % of cored section)

Oldest sediment cored: early Oligocene

Lithologies: nannofossil chalk, limestone (sediments), basalt (basement).

Tool used: LSS (Long Spacing Sonic

Recording mode: depth-derived, borehole compensated mode

Remarks about the recording: the sonic waveforms were digitized by Schlumberger on tape during Pass 2. 3, and 4 of the LSS/GR. The waveforms carry the notation that they are not on depth with each other and with the other logs. Therefore, it is recommended to first process the sonic waveforms and then depth-match the output to the logs from other runs.

Each of the four waveforms consists of 512 samples and is recorded at a sampling rate of 0.1524 m. The original data is first loaded on a Sun system using GeoFrame software. The waveform data files are then converted into ASCII and finally binary format.

Each row of the binary file is composed of the entire waveform set recorded at each depth, preceded by the depth. In the general case of 4 waveforms with 512 samples per waveform, this corresponds to 1 + 4x512 = 2049 columns. In this hole, the specifications of the files are:

Number of columns: 2049

Number of rows: 529 (Pass 2,)

Number of rows: 524 (Pass 3)

Number of rows: 263 (Pass 4)

All values are stored as ' IEEE floating point numbers' (= 4 bytes).

Any numerical software or programing language (matlab, python,...) can import the files for further analysis of the waveforms.

The following files were converted:

LSS from LSS/GR Pass 2. 3 and 4

564-p2.bin: 4098.8-4179.27 mbrf

564-p3.bin: 4090.72-4170.43 mbrf

564-p4.bin: 4139.95-4179.88 mbrf

The sonic waveform files are not depth shifted to a reference run or to the seafloor. For depth shift to the sea floor, please refer to the DEPTH SHIFT section in the standard log documentation file.

Also, please refer to the 'Remarks about the recording' note above.

NOTE: For users interested in converting the data to a format more suitable for their own purpose, a simple routine to read the binary files would include a couple of basic steps (here in old fashioned fortran 77, but would be similar in matlab or other languages):

The first step is to extract the files dimensions and specification from the header, which is the first record in each file:

  open (1, file = *.bin,access = 'direct', recl = 50) <-- NB:50 is enough to real all fields

  read (1, rec = 1)nz, ns, nrec, ntool, mode, dz, scale, dt

  close (1)

The various fields in the header are:
      - number of depths
      - number of samples per waveform and per receiver
      - number of receivers
      - tool number (0 = DSI; 1 = SonicVISION; 2 = SonicScope; 3 = Sonic Scanner; 4 = XBAT; 5 = MCS; 6 = SDT; 7 = LSS; 8 = SST; 9 = BHC; 10 = QL40; 11 = 2PSA)
      - mode (1 = Lower Dipole, 2 = Upper Dipole, 3 = Stoneley, 4 = Monopole)
      - vertical sampling interval *
      - scaling factor for depth (1.0 = meters; 0.3048 = feet) *
      - waveform sampling rate in microseconds *

All those values are stored as 4 bytes integers, except for the ones marked by an asterisk, stored as 4 bytes IEEE floating point numbers.

Then, if the number of depths, samples per waveform/receiver, and receivers are nz, ns, and nrec, respectively, a command to open the file would be:

  open (1, file = *.bin, access = 'direct', recl = 4*(1 + nrec*ns))

Finally, a generic loop to read the data and store them in an array of dimension nrec × ns × nz would be:

  do k = 1, nz

    read (1, rec = 1+k) depth(k), ((data(i,j,k), j = 1,ns), i = 1,nrec)

  enddo

For further information about the logs please contact:

Cristina Broglia

phone: 845-365-8343

fax: 845-365-3182

email: Cristina Broglia