<p>By midpoint range he refers to the size (length in the crossline direction) of the area in the subsurface that is illuminated by one pass of the boat. In a simple case of flat and parallel layers, that range is half of the size of the "spread" or receiver patch. BTW, this is true both in inline or crossline directions. </p>

<p>By coverage he means how the subsurface is illuminated by the combination of many passes of the patch over the area of a 3D survey. In common practice, passes are overlapped in the surface by half the crossline size of the patch so that the areas of subsurface illumination are contiguous with no overlap.</p>

CC BY-SA 3.0
2016-11-30T22:16:28.883Z
2016-12-01T01:52:48.210Z
2016-12-01T01:52:48.210Z
Gabriel Perez
<p>Crossline coverage is 1/2 the spread width. A survey is usually designed to deliver perfectly abutted crossline coverage (overlapping the spreads as the previous correspondent said). Common midpoint (CMP) bin width is 1/2 the cable spacing and is sampled by one source-to-receiver ray path so crossline fold by definition is one.</p>

<p>Easiest thing is to draw a diagram for yourself of a boat and spread sailing away from your page and then towards...</p>

<p>For example we had a recent survey with 13 cables at 75 m separation = 975 m spread width, so crossline coverage was 487.5 m and CMP bin width 37.5 m.</p>

CC BY-SA 4.0
2020-03-10T09:44:22.923Z
2020-03-10T10:09:21.933Z
2020-03-10T10:09:21.933Z
E L
<p>On page 29 of the book <a href="https://books.google.com/books?id=tRMiJ94mZE0C&amp;printsec=frontcover&amp;source=gbs_ge_summary_r&amp;cad=0#v=onepage&amp;q&amp;f=false" rel="noreferrer">3D Seismic Survey Design by Gijs O. Vermeer</a>, Vermeer says that the equation for a maximum fold in a 3D survey is the following:</p>

<p>$M = M_i \times M_c$</p>

<p>where $M_i$ is the inline fold and $M_c$ is the crossline fold. For a towed streamer, the inline fold is the same as for a 2D geometry which can be expressed as:</p>

<p>$M_{i} = \frac{N_{chan}\Delta r}{2\Delta s}$.</p>

<p>For the crossline fold he states that:</p>

<p><em>"The midpoint range in the crossline direction of one boat pass equals the number of streamers times the streamer interval divided by two ... normally, the next boat pass is shifted in the crossline direction with this distance, ensuring adjacent midpoint ranges of neighboring boat passes, i.e., no overlap in midpoint coverage between boat passes; hence, crossline fold $M_c = 1$. Therefore, in marine streamer acquisition, usually</em> $M = M_i$ "</p>

<p>I feel that I understand why the inline fold is the same for the case of a 2D acquisition geometry, but I am having difficulty understanding the concept of the crossline fold. Specifically from the previous quote, could someone help me to understand what Vermeer means when he says midpoint range and coverage?</p>

<p>Any help will be greatly appreciated.</p>

<geophysics><seismology><seismic>
Cross-line fold of a towed-streamer survey
geofisica
# Cross-line fold of a towed-streamer survey

(Asked by: username_0 on 2015-12-06)

On page 29 of the book [3D Seismic Survey Design by Gijs O. Vermeer](https://books.google.com/books?id=tRMiJ94mZE0C&printsec=frontcover&source=gbs_ge_summary_r&cad=0#v=onepage&q&f=false), Vermeer says that the equation for a maximum fold in a 3D survey is the following:

$M = M\_i \times M\_c$

where $M\_i$ is the inline fold and $M\_c$ is the crossline fold. For a towed streamer, the inline fold is the same as for a 2D geometry which can be expressed as:

$M\_{i} = \frac{N\_{chan}\Delta r}{2\Delta s}$.

For the crossline fold he states that:

*"The midpoint range in the crossline direction of one boat pass equals the number of streamers times the streamer interval divided by two ... normally, the next boat pass is shifted in the crossline direction with this distance, ensuring adjacent midpoint ranges of neighboring boat passes, i.e., no overlap in midpoint coverage between boat passes; hence, crossline fold $M\_c = 1$. Therefore, in marine streamer acquisition, usually* $M = M\_i$ "

I feel that I understand why the inline fold is the same for the case of a 2D acquisition geometry, but I am having difficulty understanding the concept of the crossline fold. Specifically from the previous quote, could someone help me to understand what Vermeer means when he says midpoint range and coverage?

Any help will be greatly appreciated.

**Tags:** geophysics, seismology, seismic


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## 2 answers

### Answer by username_1 on 2016-11-30. Score: 2

By midpoint range he refers to the size (length in the crossline direction) of the area in the subsurface that is illuminated by one pass of the boat. In a simple case of flat and parallel layers, that range is half of the size of the "spread" or receiver patch. BTW, this is true both in inline or crossline directions.

By coverage he means how the subsurface is illuminated by the combination of many passes of the patch over the area of a 3D survey. In common practice, passes are overlapped in the surface by half the crossline size of the patch so that the areas of subsurface illumination are contiguous with no overlap.


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### Answer by username_2 on 2020-03-10. Score: 2

Crossline coverage is 1/2 the spread width. A survey is usually designed to deliver perfectly abutted crossline coverage (overlapping the spreads as the previous correspondent said). Common midpoint (CMP) bin width is 1/2 the cable spacing and is sampled by one source-to-receiver ray path so crossline fold by definition is one.

Easiest thing is to draw a diagram for yourself of a boat and spread sailing away from your page and then towards...

For example we had a recent survey with 13 cables at 75 m separation = 975 m spread width, so crossline coverage was 487.5 m and CMP bin width 37.5 m.


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