Author Topic: KOLA BOREHOLE  (Read 425 times)


  • Administrator
  • Full Member
  • *****
  • Posts: 222
    • View Profile
« on: March 15, 2017, 05:22:30 pm »
... The hole reached 12,262 m (40,230 ft) in 1989. In that year, the hole depth was expected to reach 13,500 m (44,300 ft) by the end of 1990 and 15,000 m (49,000 ft) by 1993.[6][7] However, because of higher-than-expected temperatures at this depth and location, 180 °C (356 °F) instead of expected 100 °C (212 °F), drilling deeper was deemed infeasible and the drilling was stopped in 1992.[5] With the projected further increase in temperature with increasing depth, drilling to 15,000 m (49,000 ft) would have meant working at a temperature of 300 °C (570 °F), where the drill bit would no longer work.
... To scientists, one of the more fascinating findings to emerge from this well is that no transition from granite to basalt was found at the depth of about 7 km (4.3 mi), where the velocity of seismic waves has a discontinuity. Instead the change in the seismic wave velocity is caused by a metamorphic transition in the granite rock. In addition, the rock at that depth had been thoroughly fractured and was saturated with water, which was surprising. This water, unlike surface water, must have come from deep-crust minerals and had been unable to reach the surface because of a layer of impermeable rock. Another unexpected discovery was a large quantity of hydrogen gas; the mud that flowed out of the hole was described as "boiling" with hydrogen.

Gordon & Brigit, The following seems to show that the 12 km deep Kola borehole project found mostly igneous rock nearly all the way down. There are some thin layers of sedimentary rock down to 6 km and a very thin layer at 7 km. There may be some melted metamorphic rock that was formerly sedimentary down to 7 km. Then it's just metamorphic rock that was formerly igneous, i.e. granite below 7 km (or below 4.4 miles). Gordon, do you have comments on this?
Data on the Kola Superdeep Borehole
0-1k) Augite Diabases with Pyroxene & Porphyrites
----- ([Igneous] Diabase = subvolcanic rock equivalent to volcanic basalt or plutonic gabbro)
0>1k, 2>4k) Basic Tuffs & Tuffites
----- ([Igneous] predominantly pyroclasts = volcanic ash)
0>2k) Phyllites, Silkstones with Tuff layers
----- ([Metamorphic/Sedimentary] from shale, silt etc)
0>3k) Gabbro-Diabases
----- ([Igneous] See Diabase above)
0>3k) Laminated Sandstones
----- ([Sedimentary] from sand)
0>3-5k) Achnolitic Diabases
----- ([Igneous] See Diabase above)
0>5+6k) Dolomites, polynistic Sandstones
----- ([Sedimentary] from lime & sand)
4>5k) Sericitic Schists
----- ([Metamorphic] possibly from melted/hardened sand or shale)
3>5-6k) Metadiabases
----- ([Metamorphic] diabase from [Igneous]: see Diabase above)
5>6-7k) Diabase Porphyrites & Schists
----- ([Igneous] See Diabase above; & [Metamorphic] see Schists above)
6>7k) Conglomerates
----- ([Sedimentary] from cemented rounded rocks, larger than sand grains)
6>7-12k) Muscovite-biotite-plagioclase gniesses with high alumina content minerals
-AND Epidote-biotite-plagioclase gniesses with amphibolites, amphibolite schists & ultramafites
----- ([Metamorphic] from Igneous granite or Sedimentary rock)
_ _ _ _ _ _ _ _ _ _ _ _ _ _ Postby webolife» Tue Jan 12, 2016 3:51 am
The bore hole sampling confirms my assertion that the strata below Cambrian are primordial, ie. original crust modified when the first continent raised up above the global sea in Day 2, an event which would have been accompanied by erosion and initial depositional sequences, along with igneous upheaval and intrusive/granitic formation, and "country" rock metamorphism due to pressure and heat. Since life first appeared on the surface of this continent, it is expected that there would be limited fossils found in the "surface" layers of the "Pre-Cambrian".

It can be envisaged that continuous planetary degassing and related reorganization of the Earth’s interior mass has modified both the internal and the outer regions of the Earth progressively since early Archaean time – transforming an initially thick proto-crust as well as progressively, and episodically, increasing the volume of surface water (cf. Storetvedt, 2003 and 2011). The gradual accumulation of fluids and gases in the upper mantle and lower crust must have led to a considerable increase in the confining pressure at these levels. At each depth level, rocks and fluids would naturally be subject to a common pressure – producing a kind of high pressure vessel situation – with fractures being kept open just like those in near-surface rocks at low pressures (Gold’s pore theory, see Hoyle, 1955; Gold, 1999). This principle is well demonstrated in the Kola and KTB (S. Germany) deep continental boreholes (which reached maximum depths of 12 and 9 km, respectively) where open fractures filled with hydrous fluids were found throughout the entire sections drilled (e.g., Möller et al., 1997; Smithson et al., 2000); brines were seen to coexist with crustal rocks and, in the KTB site, the salinity of the formation water turned out to be about twice that of present-day normal sea water (Möller et al., 2005). In both drill sites, a variety of dissolved gases and fluids was found; primitive helium was observed at different depth levels indicating that the fluids were of deep interior origin (Smithson et al., 2000). As there is no observational evidence that deep oceanic depressions existed prior to the middle-late Mesozoic (see below), the bulk of present-day surface water must, in fact, have been exhaled from the deep interior during later stages of the Earth’s history. Nevertheless, there are reasons for believing that most of the planet’s water is still residing in the deep interior.

The superdeep Kola drill hole (to a depth of some 12 km) gave the surprising results that fracture spacing increases exponentially versus depth in the upper crust, and similar unexpected observations have been obtained in the 9 km deep crustal drilling site in SE Germany (KTB). A most unexpected discovery of the two continental sections was that the characteristic system of open fractures was filled with hydrous fluids which, under pressure and temperature conditions predicted for the middle and lower crust, would be in its strongly buoyant supercritical state (cf. Storetvedt, 2013 for references and discussion); hence, the strong buoyancy of supercritical hydrous fluids is likely to be the main cause of the increasing fracture volume versus depth in the continental crust. In fact, it appears that the crust does not represent a solid carapace but constitutes rather a highly fractured and increasingly fluid/gas-filled cover layer. Thus, even for the upper crust, the shear strength is likely to be much lower than what traditionally has been assumed. Accordingly, conventional estimates of tectonic twisting forces are clearly outdated; such guesses have little, if any, significance.
Unexpected discoveries from the world’s deepest well
- Hot mineralized water was found almost everywhere along the drill path.
- Helium, hydrogen, nitrogen, and even carbon dioxide (from microbes) were found all along the borehole.
- There is no basalt under the continent’s granite. This was a huge surprise. Seismic suggested that at 9,000 metres the granite would give way to basalt. It doesn’t. The seismic anomaly that suggested basalt was caused by metamorphosed granite instead.
- There are fossils in granite 6,700 metres below the surface.
The most intriguing discovery made by the Kola Superdeep Borehole researchers was the detection of microscopic plankton fossils four miles beneath the surface of the earth. Usually fossils can be found in limestone and silica deposits, but these "microfossils" were encased in organic compounds that remained surprisingly intact despite the extreme pressures and temperatures of the surrounding rock.
... the most intriguing discovery made by the Kola borehole researchers is undoubtedly the detection of biological activity in rocks more than two billion years old. The clearest evidence of life came in the form of microscopic fossils: the preserved remains of twenty-four species of single-cell marine plants, otherwise known as plankton. Usually fossils can be found in limestone and silica deposits, but these “microfossils” were encased in organic compounds that remained surprisingly intact despite the extreme pressures and temperatures of the surrounding rock.
... While the temperature gradient conformed to predictions down to a depth of about 10,000 feet, temperatures after this point increased at a higher rate until they reached 180 °C (or 356 °F) at the bottom of the hole. This was a drastic difference from the expected 100 °C (212 °F). Also unexpected was a decrease in rock density after the first 14,800 feet. Beyond this point the rock had greater porosity and permeability which, paired with the high temperatures, caused the rock to behave more like a plastic than a solid and made drilling near impossible.
Scientists found microscopic fossils of single-celled organisms at 4.3 miles (7 kilometers) down. And at nearly the same depth, they discovered water. They also found that the temperature at the bottom of the hole reached a blistering 356°F (180°C). Too hot to continue, drilling officially halted in 1994.
... geologists had expected to find a transition from granite to basalt rock at the point where the upper and lower layers of the earth’s crust intersect, about 23,000 feet down (7,000 meters). Instead, samples revealed nothing but granite until drilling ceased, much deeper than anticipated. Drilling also uncovered water at around 23,000 feet. Theoretically, this was not possible, but scientists hypothesized that this was due to oxygen and hydrogen atoms being forced together into water molecules due to the intense pressure at such depths, and then trapped by the rock layer above. The team also uncovered ancient microfossils of 24 different single-celled planktons, a fascinating discovery made all the more remarkable by the fact that the fossils were preserved in such extremes of heat and pressure.
Another unexpected find was a menagerie of microscopic fossils as deep as 6.7 kilometers below the surface. Twenty-four distinct species of plankton microfossils were found, and they were discovered to have carbon and nitrogen coverings rather than the typical limestone or silica. Despite the harsh environment of heat and pressure, the microscopic remains were remarkably intact.

« Last Edit: March 15, 2017, 06:36:20 pm by Admin »