A | This mineral is Anthropogenic. |
G | This mineral is directly dated. |
B | This mineral is reported as having this age. |
Y | This mineral is using an age reported as an element mineralization period. |
O | This mineral is using an age calculated from all data at the locality. |
R | The age displayed for this mineral originates from a different, non-child locality. |
P | The age displayed for this mineral is the range of ages for this mineral at all of this locality's children. |
This mineral's age has not yet been recorded. |
Amphibole | Apatite | Aragonite | Axinite | Baryte | Beryl | Calcite | Clinozoisite | Corundum | Epidote |
Feldspar | Gypsum | Natrolite | None | Prehnite | Pyroxene | Quartz | Rutile | Titanite | Tourmaline |
Vesuvianite | Zircon |
Mineral name | Structural Groups | IMA Formula | Max Age (Ma) | Min Age (Ma) | # of Sublocalities containing mineral | LOCALITY IDs, not mindat ids | # of localities containing mineral |
---|---|---|---|---|---|---|---|
Actinolite (*) | Amphibole | Ca2(Mg4.5-2.5Fe2+0.5-2.5)Si8O22(OH)2 | 55 | 4.5 | 1 | 95398 | 3419 |
Albite (*) | Feldspar | Na(AlSi3O8) | 55 | 4.5 | 2 | 95398,95399 | 8803 |
Aragonite (*) | Aragonite | Ca(CO3) | 55 | 4.5 | 0 | 3250 | |
Axinite-(Fe) (*) | Axinite | Ca4Fe2+2Al4[B2Si8O30](OH)2 | 55 | 4.5 | 1 | 95398 | 260 |
Baryte (*) | Baryte | Ba(SO4) | 55 | 4.5 | 1 | 95398 | 11547 |
Bavenite (*) | None | Ca4Be2+xAl2-xSi9O26-x(OH)2+x (x = 0 to 1) | 55 | 4.5 | 0 | 255 | |
Beryl (*) | Beryl | Be3Al2Si6O18 | 55 | 4.5 | 1 | 95399 | 4286 |
Calcite (*) | Calcite | Ca(CO3) | 55 | 4.5 | 1 | 95398 | 27770 |
Clinozoisite (*) | Clinozoisite Epidote | Ca2Al3[Si2O7][SiO4]O(OH) | 55 | 4.5 | 1 | 95398 | 1025 |
Diopside (*) | Pyroxene | CaMgSi2O6 | 55 | 4.5 | 1 | 95398 | 4135 |
Dolomite (*) | None | CaMg(CO3)2 | 55 | 4.5 | 0 | 9895 | |
Epidote (*) | Epidote Clinozoisite | Ca2(Al2Fe3+)[Si2O7][SiO4]O(OH) | 55 | 4.5 | 1 | 95398 | 8173 |
Fluorapatite (*) | Apatite | Ca5(PO4)3F | 55 | 4.5 | 1 | 95399 | 2740 |
Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 55 | 4.5 | 1 | 95398 | 6890 |
Hematite (*) | Corundum | Fe2O3 | 55 | 4.5 | 0 | 14640 | |
Microcline (*) | Feldspar | K(AlSi3O8) | 55 | 4.5 | 1 | 95399 | 4924 |
Natrolite (*) | Natrolite | Na2(Si3Al2)O10·2H2O | 55 | 4.5 | 1 | 95398 | 1236 |
Orthoclase (*) | Feldspar | K(AlSi3O8) | 55 | 4.5 | 0 | 2349 | |
Prehnite (*) | Prehnite | Ca2Al(Si3Al)O10(OH)2 | 55 | 4.5 | 0 | 1898 | |
Quartz (*) | Quartz | SiO2 | 55 | 4.5 | 3 | 95398,95399,95400 | 61156 |
Rutile (*) | Rutile | TiO2 | 55 | 4.5 | 1 | 95398 | 5614 |
Schorl (*) | Tourmaline | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 55 | 4.5 | 1 | 95399 | 2705 |
Siderite (*) | Calcite | Fe(CO3) | 55 | 4.5 | 1 | 95398 | 6417 |
Titanite (*) | Titanite | CaTi(SiO4)O | 55 | 4.5 | 1 | 95398 | 4899 |
Tremolite (*) | Amphibole | Ca2(Mg5.0-4.5Fe2+0.0-0.5)Si8O22(OH)2 | 55 | 4.5 | 1 | 95398 | 2562 |
Vesuvianite (*) | Vesuvianite | (Ca,Na)19(Al,Mg,Fe)13(SiO4)10(Si2O7)4(OH,F,O)10 | 55 | 4.5 | 1 | 95398 | 1395 |
Zircon (*) | Zircon | Zr(SiO4) | 55 | 4.5 | 0 | 5251 | |
Zoisite (*) | Epidote | Ca2Al3[Si2O7][SiO4]O(OH) | 55 | 4.5 | 1 | 95398 | 1025 |
Age ID | Locality Notes |
---|---|
AJG8_9877_001 | The Dassu orthogneiss hosts many pegmatites, Gilgit is the location of several of these pegmatites |
AJG8_9877_002 | The Dassu orthogneiss hosts many pegmatites, Gilgit is the location of several of these pegmatites |
AJG8_9877_003 | Shigar Valley pegmatites |
Excel ID | Max Age (Ma) | Min Age (Ma) | Age as listed in reference | Dating Method | Age Interpret | Prioritized? | Sample Source | Sample Num | Run Num | Age from other Locality | Dated Mineral | Minerals explicitely stated as having this age | Age applies to these Elements | MinDat Locality ID | Dated Locality (Max Age) | Location as listed in reference | Reference | Reference DOI | Reference ID | Age Notes | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
AJG8_9877_001 | 7.4 | 6.8 | 7.1±0.3 | Yes | 2530 | Gilgit, Gilgit District, Gilgit-Baltistan, Pakistan | Dassu orthogneiss | Agheem et al. (2015) | 10.1007/s12517-015-1900-x | AJG8_9877 | The age of the pegmatites is younger than the Dassu orthogneiss which hosts them, there is no metamorphic overprint on the pegmatites | ||||||||||
AJG8_9877_002 | 4.9 | 4.5 | 4.7±0.2 | Yes | 2530 | Gilgit, Gilgit District, Gilgit-Baltistan, Pakistan | Dassu orthogneiss | Agheem et al. (2015) | 10.1007/s12517-015-1900-x | AJG8_9877 | The age of the pegmatites is younger than the Dassu orthogneiss which hosts them, there is no metamorphic overprint on the pegmatites | ||||||||||
AJG8_9877_003 | 55 | 50 | 55-50 | age of collision | Yes | 2530 | Gilgit, Gilgit District, Gilgit-Baltistan, Pakistan | Shigar Valley pegmatites | Agheem et al. (2015) | 10.1007/s12517-015-1900-x | AJG8_9877 | Trace elements variations place the Shigar Valley pegmatites into syn-collision granite domain. This collision-related magmatism took place when Indian plate collided with the Eurasian plate ~55 to 50 Ma ago (e.g., Molnar and Tapponnier 1975; Petterson and Windley 1985; Beck et al. 1995; Rowley 1996; Bignold and Treloar 2003; Rehman et al. 2011) |
Sample | Source Locality | Reference URL |
---|---|---|
R110128 | Alchuri (Alchori; Aschudi), Shigar District, Gilgit-Baltistan, Pakistan | https://rruff.info/R110128 |
R110127 | Alchuri (Alchori; Aschudi), Shigar District, Gilgit-Baltistan, Pakistan | https://rruff.info/R110127 |
R060935 | Alchuri (Alchori; Aschudi), Shigar District, Gilgit-Baltistan, Pakistan | https://rruff.info/R060935 |
All locality data graciously provided by mindat.org
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