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This is a more elaborate version of the AVO anomalies including both the Top of Sand and Base of Sand version. And here is a summary of AVO classes I posted earlier in case you missed it. https://lnkd.in/dGmgfweu
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https://lnkd.in/gkFFm_HK News is out for the #Gold in porphyry intrusion at Silverback! The grades are modest, however "gold is where you find it", and now we have a clear vector and plan to explore for the larger intrusive source to this blind hit and the high grade copper-gold-silver shear zones exposed by stripping overburden. When Byron told me he found crystalline molybdenite at Silverback, along with the 9.5g/t gold, 5.6% copper and 49.5 g/t silver nearby, I knew there was something special going on. Many researchers have pointed out that Hemlo isn't an orogenic gold system but is rather intrusion related, with strong hydrothermal elements, that had subsequently been metamorphosed focusing gold and molybdenum into high grade shear zones. The story at Silverback is early, but the ingredients for a similar system are coming together nicely! 3D array IP geophysics and Drilling this fall and winter are planned.
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RQD Index: It helps us assess the integrity of rock core samples, determining fracture frequency and overall rock stability. #GeotechnicalEngineering #RockQuality #RQD #Geotech #EngineeringInnovation #drilling #geotechnicaldrilling #driller #metadrill
Rock Quality Designation (RQD) Index https://lnkd.in/dCB6brXs
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7moThe AVO crossplot actually represents fluid, lithology and porosity at the same time. The polygon around the background represents shales and wet sands. As you move away from the background you will have where oil will plot and even further away it is where natural gas will plot. The volume you create from these polygons will represent fluid, lithology and porosity. If we lay this over the seismic we should see where the AVO anomalies match structure. If they match structure we can further de-risk the anomaly. We can also output this volume and use it the Geomodel to create seismic facies. Seismic facies is what we want to use in our Geomodel. We can then take this data and invert it which will improve our resolution since we are removing sidelobes with the well model and increasing the resolution by phase rotating -90 degees. The wavelet now represents a rock property. We can then use a crossplot of inversion attributes to again create seismic facies. Once we have done the seismic inversion can use neural net to create a rock properties that matches the well logs. This volume could be porosity (porosity), gamma Ray and Archie’s fluid volumes.