VẬT lý địa CHẤN 07 field

16 936 0
VẬT lý   địa CHẤN 07 field

Đang tải... (xem toàn văn)

Tài liệu hạn chế xem trước, để xem đầy đủ mời bạn chọn Tải xuống

Thông tin tài liệu

• • • • • • • Common-offset & Zero-offset Common-midpoint method Up-dip and down-dip shooting Spread types Singlefold / Multifold recording Crooked line method Determining field parameters Common-Offset X Source and Receiver have always the same distance Moveout must be taken into account or corrected for Zero-Offset X Source and receiver are at the same location (i.e the offset is zero -> “zero offset”) => No Move-out CMP - “ Common Mid Point” CMP = CDP CMP ¹ CDP CMP = common mid point CDP = common depth point +●●●●●●●● Down-dip shooting ● ● ●● ● ●● ●+ Up-dip shooting Remember the refraction measurement where both shooting directions were needed to estimate the velocity of the lower layer Common field layouts +●●●●●●●●● split spread ●●●●●● ●●●●●● single ended (inline offset) + ●●●●●●●●● fan shooting + ●●●●●● + ●●●●●● + ●●● ●●● ●●● single ended (end on) (Top view) roll along more Geophones in the Field than active channels +●●●●●●●●● ●●●●●●●●● active not-active ● + ●●●● ●●●● ● ●●● ●●●● ● active ● ●●● ●● ● + ●● ●●● ●●● ● ●● active Geometry of Geophones relative to the source remains the same “roll along acquisition” ●●●●●●●●●●●●●●● ● ● ●●●●●●●● ●●●●●●● ●● ●●●●●●●● ●●●●●● ●●● ●●●●●●●● ●●●●● ●●●●●●●●●●●● ●●●● ●●●●●●●●●●●●● ●●● ●●●●●●●●●●●●●● ●● ● ● active not-active Sources and receivers on a road Resulting line From Sheriff, 1995 From Reynolds, 1997 Xo=(Xs-Xr)/2 Xm=(Xs+Xr)/2 From Reynolds, 1997 ● ● ● ● ● ● ● ● ● ● + ● ● ● ● ● ● + ● ● + ● ● + ● ● + ● ●+ ● + No geophones: 4, distance geoph: 1, distance source: 1, Fold: + No geophones: 4, distance geoph: 1, distance source: 2, Fold: ● ● ●● ● ●● ● ●● ● ● + ●● ● ●● ● ●● ● ●● ● + ● ●● ● ●● ● ● ●● ● ● ● ● ●● ● ● ●● ● ● ● ● + + ●● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ●●● + + Coverage (“fold”) Number of traces per CMP Number of geophones * Distance between the geophones Fold = * Distance between the shots Coverage = Fold *100% From Reynolds, 1997 • Maximum offset » Depth deepest zone of interest • Minimum offset » Not greater than shallowest section of interest • Maximum array length is determined by the minimum apparent velocity of reflections • Charge size determined by ambient noise late on the record • Line orientation (up-dip, down-dip) ... offset is zero -> “zero offset”) => No Move-out CMP - “ Common Mid Point” CMP = CDP CMP ¹ CDP CMP = common mid point CDP = common depth point +●●●●●●●● Down-dip shooting ● ● ●● ● ●● ●+ Up-dip shooting...Common-Offset X Source and Receiver have always the same distance Moveout must be taken into account or corrected for Zero-Offset X Source and receiver are at the... single ended (end on) (Top view) roll along more Geophones in the Field than active channels +●●●●●●●●● ●●●●●●●●● active not-active ● + ●●●● ●●●● ● ●●● ●●●● ● active ● ●●● ●● ● + ●● ●●● ●●● ●

Ngày đăng: 08/12/2016, 20:27

Từ khóa liên quan

Tài liệu cùng người dùng

Tài liệu liên quan