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Sunday, September 11, 2011 at 07:27:45 AM at epicenter
Magnitude
4.4
Depth
10.3 km (6.4 miles)
126 km (78 miles) SE of Lubbock, Texas
The Permian Basin gives its name to a large oil and natural gas producing area, part of the Mid-Continent Oil Producing Area. Total production for that region up to the beginning of 1993 was over 14.9 billion barrels.
Originally posted by Old77
got any fracking going on there? How deep was the EQ. Epicenter?
Originally posted by Aggie Man
I will vote against fracking as the cause. My reasoning is that the quake was 6.4 miles deep and they are not drilling anywhere near that depth.
Hydraulic fracturing enables the production of natural gas and oil from rock formations deep below the earth's surface (generally 5,000-20,000 feet or 1,500-6,100 m). At such depth, there may not be sufficient porosity and permeability to allow natural gas and oil to flow from the rock into the wellbore at economic rates. Thus, creating conductive fractures in the rock is essential to extract gas from shale reservoirs because of the extremely low natural permeability of shale, which is measured in the microdarcy to nanodarcy range.[4] Fractures provides a conductive path connecting a larger area of the reservoir to the well, thereby increasing the area from which natural gas and liquids can be recovered from the targeted formation.
Originally posted by Old77
got any fracking going on there? How deep was the EQ. Epicenter?
*Yikes 6.4 miles, thats not Fracking that's Mother Nature... Even if you take into account their probability of error on the location its not Fracking..edit on 11-9-2011 by Old77 because: (no reason given)
In numerous parts of the world today, including some of the most highly developed countries, many dam designers and operators have tended to close their eyes to the engineering problems posed by reservoir-induced earthquakes. One sometimes hears these kinds of defensive arguments: (1) no convincing correlation has yet been demonstrated between earthquakes and reservoirs; (2) since the natural seismicity at a given site is low, the danger of reservoir-inducement is therefore also low; (3) the geology at a given site is different from that at localities where major reservoir-induced events have occurred; (4) only three or four out of some 11,000 large dams worldwide have experienced significant induced earthquakes, and one should therefore not worry about a given site; and (5) no dam has yet failed disastrously because of a reservoir-induced earthquake, and the danger is thus grossly exaggerated. While many of these arguments have some elements of truth to them, they are essentially evading the primary issues: Virtually every careful study has concluded that there is indeed a cause-and-effect relationship between some earthquakes and some reservoirs, and two dams (Koyna, India, and Hsinfengkiang, China) have in fact come uncomfortably close to disastrous failure during such events. Furthermore, it is precisely in the regions of low natural seismicity where the major existing problems lie, because in areas of high seismicity dams are usually designed for substantial earthquake resistance anyway.
Originally posted by muzzleflash
reply to post by marzabeth
It appears that you are proposing an alternative theory that perhaps this could be the result of a domino effect originating from something like a large body of water. This is possible, but we won't know without in depth investigation and we may need experts with better resources to aid in that process.
I recall people discussing the weight distribution of the Three Gorges Dam and how it could lead to seismic activity or even potentially altering the tilt of the Earth's axis.
There could be something to this, but it would require us to identify a location and show how it lead to a quake 6 miles underground, which will likely prove exceedingly difficult.
I am open to a possibility like this but it will require a lot of work to substantiate it.
A fluid injection-induced seismicity experiment was conducted in the German Continental Deep Drilling Program (KTB) main borehole at 9.1 km depth (in situ temperature of 260°C) to extend knowledge about stress magnitudes and brittle faulting to depths and temperatures approaching the brittle-ductile transition. Almost 400 microearthquakes were induced at an average depth of 8.8 km by injection of KBr/KCl brine into a ∼70 m open hole section near the bottom of the borehole.