Presentation on theme: "8. Ocean Crustal Structure and Seismic Reflection William Wilcock (via Michelle W.) OCEAN/ESS 410."— Presentation transcript:
8. Ocean Crustal Structure and Seismic Reflection William Wilcock (via Michelle W.) OCEAN/ESS 410
Lecture/Lab Learning Goals Know the basic structure of the oceanic crust as determined from ophiolite studies Understand how oceanic crustal structure is linked to mantle melting and volcanic processes Physics: Understand what seismic impedance is and how it controls the amplitude of seismic reflections Data collection: airguns & LOTS of hydrophones Data processing: Be able to explain how reflection data is stacked and converted into a seismic record section Interpretation: What can seismic records tell you? (LAB)
The Geology part: Ophiolites Ophio = Snake (i.e. green) Lithos = Stone
What if the Juan de Fuca Ridge collided with the North American Plate? North American Plate Juan de Fuca Ridge I’m so hungry! I think I’ll eat the whole Juan de Fuca plate. Nom nom nom Oh no! Please don’t eat me!
What if the Juan de Fuca Ridge collided with the North American Plate? North American Plate Juan de Fuca Ridge I’m so hungry! I think I’ll eat that Mid Ocean Ridge. Nom nom nom Oh no! Please don’t eat me! You would get an ophiolite! -Often happens when ocean basins close -You get “obduction”, or upthrust of oceanic crust and mantle onto continental plates
Reflections from Interfaces When a downgoing P-wave meets an interface, a portion of the wave is reflected.
Characteristic acoustic impedance -An inherent property of the medium -Depends on sound speed (or seismic velocity) and density -Pressure generated by vibration of molecules of a particular medium at a given frequency
Amplitudes of Reflections for vertical rays A0A0 V 1, 1 V 2, 2 The amplitude of the reflected and transmitted phase depends on the seismic velocity, V and the density, in each layer. Larger contrasts in impedance result in large amplitude reflections
Marine Reflection Seismology - Airgun Sources Reflection data is relatively easy to acquire in the oceans. Seismic sounds (shots) can be generated with arrays of compressed air guns (airguns) towed behind the ship
Marine Reflection Seismology - Hydrophone Streamers The airgun shots are recorded by arrays of hydrophones towed behind the ship in a streamer. The seismic streamers contain 1000’s of hydrophones and can be >10 km long. A modern 3-D seismic ship will tow several (the records is 20) streamers.
Marine Reflection Seismology - Geometry The streamer records waves reflected from interfaces
Marine Reflection Seismology - Data The seismic data recorded for a particular shot will display a geometric effect termed “normal moveout” (NMO) which reflects the increased distance the wave travels as source-receiver offset increases Offset Time, s Time X 0
Marine Reflection Seismology - Sorting Records The records are sorted so that they all have the same mid-point (Common Mid-Point - CMP)
Marine Reflection Seismology - Airgun Sources The seismic records can be corrected for geometric affects and stacked (summed) to produce a single record for the reflections below each each point Before Geometric Correction After Geometric Correction Stacked (summed)
Marine Reflection Seismology - Filled Wiggle Plots Stacked records are plotted on the same plot with the horizontal axis showing position along the profile. Rather than showing lines for each record the plots often show filled regions for positive (or negative) displacements Time, s Position
A reflection profile across the East Pacific Rise Reflections come from the seafloor, the base of layer 2A (pillow basalts), the axial magma chamber (AMC) and the Moho (M)