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| -1.3+(42.5-7)= 34.2 Ma-ago ||Phanerozoic{Paleogene.Oligocene <sup>#</sup> Paleogene.Eocene}:33.9Ma-ago
| -1.3+(42.5-7)= 34.2 Ma-ago ||Phanerozoic{Paleogene.Oligocene <sup>#</sup> Paleogene.Eocene}:33.9Ma-ago
|-
|-
| 34.2+36 = 70.2 Ma-ago || Phanerozoic{Cretacious.Maastrichtian}:72.1(±0.6)Ma-ago*
| 34.2+36 = 70.2 Ma-ago || Phanerozoic{Cretacious.Maastrichtian}:70.6(+0.4)Ma-ago*
|-
|-
| 70.2 + 75 = 145.2Ma-ago ||Phanerozoic{Jurassic – Cretaceous}:145(±4)Ma-ago
| 70.2 + 75 = 145.2Ma-ago ||Phanerozoic{Jurassic – Cretaceous}:145.5(-0.3)Ma-ago
|-
|-
| 145.2 + 54 = 199.2Ma-ago || Phanerozoic{Triassic – Jurassic}:201(±0.6)Ma-ago
| 145.2 + 54 = 199.2Ma-ago || Phanerozoic{Triassic – Jurassic}:199.6(-0.4)Ma-ago
|-
|-
| 199.2+(42.5+7)= 248.7 Ma-ago || Phanerozoic{Permian <sup>#</sup> Triassic}:251Ma-ago</br>
| 199.2+(42.5+7)= 248.7 Ma-ago || Phanerozoic{Permian <sup>#</sup> Triassic}:251Ma-ago(-2.3)</br>
|-
|-
|248.7+36 = 284.7Ma-ago || Phanerozoic{Carboniferous – Permian}:286 vs 298 Ma-ago*
|248.7+36 = 284.7Ma-ago || Phanerozoic{Carboniferous – Permian}:299 vs 290Ma-ago*
|-
|-
|284.7+74=358.7Ma-ago || Phanerozoic{Devonian – Carboniferous}:358.9(±2.5)Ma-ago
|284.7+74=358.7Ma-ago || Phanerozoic{Devonian – Carboniferous}:358.9(-0.2)Ma-ago
|-
|-
|358.7+57=415.7Ma-ago || Phanerozoic{Ordovician – Devonian}:419.2(±2.8)Ma-ago
|358.7+57=415.7Ma-ago || Phanerozoic{Ordovician – Devonian}:419.2(-3.5)Ma-ago
|-
|-
|415.7+(42.5-7) = 451.2Ma-ago || Phanerozoic{Ordovician <sup>#</sup> Silurian}:443.7Ma-ago**
|415.7+(42.5-7) = 451.2Ma-ago || Phanerozoic{Ordovician <sup>#</sup> Silurian}:443.7Ma-ago**
Line 116: Line 116:
ICS: International Commission on Stratigraphy</br>
ICS: International Commission on Stratigraphy</br>
<br//>
<br//>
[[User:Morbas|Morbas]] ([[User talk:Morbas|talk]]) 15:54, 14 January 2014 (UTC)
[[User:Morbas|Morbas]] ([[User talk:Morbas|talk]]) 19:24, 30 January 2014 (UTC)


== Polar MW SOL Arm Intercepts ==
== Polar MW SOL Arm Intercepts ==

Revision as of 19:24, 30 January 2014

Physical Geologic Driver

Geologic Periods are defined by a biostratigraphic process alignment of sedimentary rocks with fossil floral and assemblages. The ICS Phanerozoic Eon Geologic Time Scale documents evolution of Eukarya (animal, plant, et al.), an emergent compendium of 417 Ma covariant Period interval sets. These are HoloceneR - SilurianS (-1 - 416 = 417 Ma-ago), OligoceneOl - OrdovicianO (28 - 444= 417 Ma-ago), MaastrichtianMaas stage - CambrianCm (71* - 488= 417 Ma-ago), JurassicJ - VendianV Ediacaran-Varangian (146 - 563= 417 Ma-ago) unconstrained date and CarboniferousC - Proterozoic Cryogenian-Ediacaran (~286 - ~703= 417 Ma-ago). The Carboniferous ends in a Karoo Ice Age, the 286 Ma-ago date is circa 1982pp5,pp114:[1] geologic dating, igneous province FN7 and a two pulse process. The Cryogenian (or Sturtian-Marinoan) Ice Age 800 to 600 Ma-ago is a two pulse process in a geologic span ~417 M-years earlier. Reiteration of the commutative 417Myr six interval setFN4 generates our Phanerozoic Period transitions. Within the commutative group (Apoapsis:Oligocene & O-S, Periapsis:P-Tr)FN5 is a subset of elevated tectonic intervals proposed by Radon & Kevet 1990 which extends out of the Phanerozoic, across the Proterozoic, through the Archaean and into Hadean to the 4.5 Ba ago Moon-forming impact[2]. The Moon stabilizes Earth's tilted spin axis with annual seasons. Mid ocean-ridge volcanism driven by the moon primordial event and Earth accretion energy regulates Ocean depth [3]. An enlarged liquid core further sustains polar magnetic shielding. [4] Hyperthermophile life spawned upward from that environment, including frequent ocean boiling stages 4.3 Ba-ago.[4] The physical environment bounded life on Earth, starting with CO2 dominated biosphere into the present Eukaryote plant and Pre-Cambrian global eukaryote photosynthesized oxygenic atmosphere.[4] The impact of 'Physical perturbations breaks incumbencies, removes dominant life forms, and opens opportunities for previous minor groups'.[4] The biological process obliges environmental shifts, fostering new phenotype exploitation of our Rare Earth and Gaia biosphere.


Period / STAGE PHYSICAL / Delta 6th Interval ISC (Ma ago) PERFN5 Big 5 ICE LIPFN7 CIEFN7
-1Ma ago A
Paleogene_Neogene Δ(79-7)M P 33.9-23Ma ago FN1 <--Mid-Oligocene
Paleogene 66(±0.3) K–Pg
MAASTRICHTIAN 70.6Ma ago B 72.1(±0.6) 72.3Ma-ago 71Ma-ago
Cretaceous Δ75M
145.5Ma ago C 145(±4.0) 147Ma-ago
Jurassic Δ54M
201.6Ma ago D 201.4(±0.6) Tr-J 198Ma-ago 200Ma-ago
Permian_Triassic Δ(79+7)M 251(±0.4) <--PTr P-Tr 251Ma-ago 252Ma-ago
~286Ma ago 298.9(±0.8) Karoo 285Ma-ago
Carboniferous Δ73M
359Ma ago 358.9(±2.5) late-D 359.2Ma-ago
Devonian Δ57M
416Ma ago A417M 419.2(±2.8) 420Ma-ago(-)
Ordovician_Silurian Δ(79-7)M P417±2M--> 443.7(±1.5)FN2 <--OS O-S
488Ma ago B417M 485.4(±1.7)
Cambrian Δ75M
~563Ma agoFN3 C417M ~538.8(±1.0)
Varangian.Ediacaran Δ54M
~617Ma ago D417M ~635
Varangian.Cryogenian
648±13 Mannoan
714±17 Sturtian
Legend
period_period : underscore shows a PER point.
~period : tilda indicates poorly constrained dates.
± : interval.
(±) : accuracy estimation.

FN1: Oligocene Epoch Interval ice notch 32.5-25.5Ma-ago
FN2: Ordovician–Silurian extinction event ice interval.
FN3: ICS 1998 http://www.palaeontologie.uni-wuerzburg.de/Stuff/casu6.htm
FN4: 417MA,B,C= commutative sum {(79-7), 75, 54, (79+7), 73, 57 }. Using only (79±7, 74, 55.5) Phanerozoic Galactic Arm Periods are mathematically expressed to ±2Ma absolute accuracy. The CB Periods (Oligocene, OS and P-Tr) are approximately at (79±7)/2 time points.
FN5: SOL CB retrograde movement causes inverse Kepler apsis SOL ISM flow rates.
FN6: Kvet PER sets uniquely divide the mid-apsis internals, thus reside close to the apsis axis. The Planetary Equidistant Rupture is otherwise a controversial record.
FN7:Large Igneous ProvinceLIP and Carbon Isotope ExcursionCIE (14C): Gillman/Erenler (2008) The galactic cycle of extinction
  1. ^ Snelling 1985 Chronology of the Geologic Record; Boston, Blackwell Scientific Publications. ISBN 0-632-01285-4
  2. ^ Radon & Kevet Complete periodical table Radon Kevet, GeoJournal 1991, Vol 24 Num 4 ppg 317-420
  3. ^ Kasting, J.F, Holm, N.G (1992). What determines the volume of the oceans? Earth and Planetary Science Letters, 109: 507-515
  4. ^ a b c d Rothschild, L.J. & A. Lister (eds.) Evolution on Planet Earth: The Impact of the Physical Environment. Academic Press. 2003. 456 pp. ISBN 0-12-598655-6

.


Morbas (talk) 17:59, 1 April 2012 (UTC)

Geologic Time Scale Pattern

Pattern ideologue Stratigraphy and ICS dating
-1.3+(42.5-7)= 34.2 Ma-ago Phanerozoic{Paleogene.Oligocene # Paleogene.Eocene}:33.9Ma-ago
34.2+36 = 70.2 Ma-ago Phanerozoic{Cretacious.Maastrichtian}:70.6(+0.4)Ma-ago*
70.2 + 75 = 145.2Ma-ago Phanerozoic{Jurassic – Cretaceous}:145.5(-0.3)Ma-ago
145.2 + 54 = 199.2Ma-ago Phanerozoic{Triassic – Jurassic}:199.6(-0.4)Ma-ago
199.2+(42.5+7)= 248.7 Ma-ago Phanerozoic{Permian # Triassic}:251Ma-ago(-2.3)
248.7+36 = 284.7Ma-ago Phanerozoic{Carboniferous – Permian}:299 vs 290Ma-ago*
284.7+74=358.7Ma-ago Phanerozoic{Devonian – Carboniferous}:358.9(-0.2)Ma-ago
358.7+57=415.7Ma-ago Phanerozoic{Ordovician – Devonian}:419.2(-3.5)Ma-ago
415.7+(42.5-7) = 451.2Ma-ago Phanerozoic{Ordovician # Silurian}:443.7Ma-ago**
451.2 + 36 = 487.2 Ma-ago Phanerozoic{Cambrian – Ordovician}:485.4(±1.7)Ma-ago
487.2 + 74 =561.2Ma-ago Varangian{Ediacaran} – Phanerozoic{Cambrian}:541***



Legend:
Geologic Convention Eon{Period.Stage}:ICS date
CB alignments #
Controversial Issues *
Ordovican.Late Ice Age from 460Ma-ago**
Cambrian Explosion was a middle Driver transition. ***
ICS: International Commission on Stratigraphy

Morbas (talk) 19:24, 30 January 2014 (UTC)

Polar MW SOL Arm Intercepts

Radius (KLyr) Theta (degrees)FN1 Arm Period
15.99 +1.12 Orion Cenozoic/Devonian
15.97 0.00 present Holocene
15.67 -29.57 CB (near) Oligocene
7.33 -29.57 CB (near end)
15.96 -61.09 Perseus Masstrichtian
15.89 -125.57 Norma-Cygnus Cretaceous
15.84 -172.93 Shaver Jurassic
16.25 -216.85 CB (far) P-Tr
7.33 -216.85 CB (far end)
15.83 -250.33 Scutum-Crux Permian
16.10 -310.67 Sagittarius Carboniferous


FN1: SOL at 0.00O Orion 1.30Myr-future; Oligocene 34Ma-ago
Ellipsis Apoapsis -30.85O from SOL, eccentricity 0.019, Period 139.35Ma, and spiral eggress 0%/135.3Ma. Ellipsis superimposed on 417Ma relative CB rotation cycle. Arm theta expansion fits to 0.18% using root sum of squares of differences. The small 7.278O CB bend WIP (looking into z Sol oscillation. GSA 2009 dates reduced disparities except using earlier dates noted.
Polar Radial Arm expansion Equation R=A * THETA2.57+RCB
RCB=7.33Klyr
RSPUR <= ASPUR=33.9Klyr Arms{Orion, Shaver}
RMINOR <= AMINOR=19.9Klyr Arms{Sagittarius,NormaSigma}
RMAJOR <= AMAJOR=11.1Klyr Arms{Scutum-Crux, Perseus}
Theta=angle(degrees)/360
Calculation advances triple radial-symmetric arm expansion patterns.
Ratios {ASPUR,AMINOR} 1.72 and {AMINOR,AMAJOR} 1.70
THETA in degrees referenced to expansion from CB near & far polar angles.

Notes: 1) Review of Raup/Sepkoski Periodicity of extinctions in the geologic past 1983 Statistical analysis was limited to 250Ma, (Sepkoski / Harland extinction data base used for various reasons), produces a 26Ma peak for time series fourier transform. My assertion is if the analysis was across the Phanerozoic, they would have found this 417Ma equal covariance. Work in progress, as the 52Ma is an octive of 417Ma within the tolerances of the 26Ma they have presented. 417/8=52.125...hmmm six MW arms plus two CB alignments yields eight Period Transitions per 417Ma passage through all the arms.
2) Raup/Sepkoski used fourier, an analysis that depends on a continous wave. They attempted to include datum across nore than 250Ms ago, but dismissed the results because of lower quality. Now we see (above) that datum over 250Ma ago slips across the near and far CB arm expansion sets. This introduces a phase shift that effects the fourier analysis quality. A secondary effect further mucks up the analysis, and that is the variations caused by unregular intercepts of the expanding MW spirals and the variation is radius of the ellipsis orbit. They did not find the 417Ma, let alone the 139Ma elliptical SOL/MW orbital overlay.
3) Regressive trace arms into the Galactic center reveals centric inner bulge/halos causality. Centric outward paired spirals, refracted by far and near CB particle beams generate dual triple arm divergence, a 2+2+2 Galactic Arm Cb structure causal. The near side beam defines our Oligocene 7 million year thermal notch. The far beam intercepts SOL at PTr.
WIP using Plasma cosmology
Morbas (talk) 17:50, 30 January 2014 (UTC)

Orbital

Proposal:
The 417Ma commutative apsis set expresses an event sampled alias:
SOL CB slipage <= 0.863O/Ma <= 360O/417Ma
29.57OCB(lead angle)<= Oligocene.Rupelian 34Ma * 0.863
SOL orbits the MW every 139.35Ma <= 417Ma/(2n*(3/2)); for n=1 : n{integer}.
SOL MW orbit spiral egress 0%, eccentricty 0.019, SOL to Apoapsis -30.85O (35.74Ma future), PTr R=15.84K Lyr, Oligocene R=15.67K Lyr, CB bend 7.278O
SOL radial velocity is 2.66O/Ma.
CB rotates at 3.523O/Ma <= (2.66O/Ma) +(0.863O/Ma).
Issues with NASAWIKIPEDIA resolved by Bremstrahlung red shift operator. WIP
CB rotation time is 102.18Ma<=360O/(3.523O/Ma)
Results:
A 139.5Ma cycle exists for a SOL orbit of the Galaxy derived from 417Ma geologic interleaved Period sets. This lends credence to:
a) Cosmic Ray Flux astrophysical 135±9Ma climatic cycle[4].
b) accounting for molecular hydrogen soft bremsstrahlung red shift indicates smaller Galaxy, and reduced SOL MW radius.
c) the 139.5 Ma geologic cycle expresses increased GCR. Per P.Frisch[1], the SOL heliosphere is modulated by Galatic ISM. Velocity and Intensity are important variables, as well as Sun activity cycles that modulate the heliosphere flow and density. Sol velocity is 370KM/Sec, a 0.019 eccentricy velocity variation is 2.4% (±8.8KM/Sec). Present Orion ISM pressures are 25KM/s. The coincidencez of mid apsis points are close to Arm intercepts. We are at one coincidencez, coming out of periapsis into apoapsis. Thus egressing from a general 70Ma interval high flow rate(cooling) into a minimum (warming) 70Ma interval. The double ice age impulses at Carboniferous Karoo and Crogenian-Ediacaran congruent with arm orbit angle minimums. The P-Tr was at apoapsis at CB while crossing the CB alignment. d) Keplar 3rd Law proportions MW mass is 0.585[±.05] for 139Ma period, and 18.3Kly Sol Radius compared to the standard model 200Ma Period 27.2Kly radius. This solves the star MW orbital cunundrum between predicted visa vis observed velocity.
Reference:
[1] "Solar Journey: The Significance of Our Galactic Environment for the Heliosphere and Earth", Springer, in press (2006), editor P. C. Frisch
[2] "Black Holes and Jets" Astronomy News email Feb 17, 2010; Evans, MIT Cambridge Maryland.
[3] "A Radio through X-Ray Study of the Jet/Companion-Galaxy Interaction in 3C 321" (2008), Astrophysics Journal, Evans, Fong and others.
[4] "Celestrial driver of Phanerozoic climate?" GSA Today July 2003, Nir J Shaviv and Jan Velzer


END


estimate of eccentricity <= = 0.05(±0.02) <=
Eccentricity revised by SOL orbital plots accounting for 24km/s variation of relative ISM velocity required to uncover Earth of moderating (temperature and Ozone depletion) heliosphere. Plots subjected to correlation with axial matching Galactic Arms expansion from each end of the CB.
This from mapping the SOL orbit, where eccentricity modulates the SOL MW 0.863O/Ma net retrograde velocity.
semi-latus rectum = p 26kly @90O ergo lateral
polar
area<=
END Morbas (talk) 00:08, 15 January 2014 (UTC)

Observation Differences

Type Wikipedia PGD[1]
MW SOL Radius 27.2Kly 15.96Kly[2]
SOL Orbital ≈238Myr 139(-)Myr[2]
MW Pattern 50Myr NA[3]
CB Rotation 15-18Myr 102Myr abs


NOTES
[1] Physical Geologic Driver (PGD)
[2] WIP
[3] The MW pattern emits from both CB ends and expands outward, crossing the SOL orbital.
Morbas (talk) 17:49, 30 January 2014 (UTC)