Knowledge

Reduced chi-squared statistic

Source ๐Ÿ“

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for each age determination. As regards weighting, one can either weight all of the measured ages equally, or weight them by the proportion of the sample that they represent. For example, if two thirds of the sample was used for the first measurement and one third for the second and final measurement,
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M. J. Streule, R. J. Phillips, M. P. Searle, D. J. Waters and M. S. A. Horstwood 2009. Evolution and chronology of the Pangong Metamorphic Complex adjacent to themodelling and U-Pb geochronology Karakoram Fault, Ladakh: constraints from thermobarometry, metamorphic modelling and U-Pb geochronology.
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MSWD > 1 if the observed scatter exceeds that predicted by the analytical uncertainties. In this case, the data are said to be "overdispersed". This situation is the rule rather than the exception in (U-Th)/He geochronology, indicating an incomplete understanding of the isotope system. Several
1052: 2039: 2454: 1554: 1794: 1549: 1401: 2731:{\displaystyle {\text{MSWD}}_{w}={\frac {\sum _{i=1}^{N}w_{i}}{{\big (}\sum _{i=1}^{N}w_{i}{\big )}^{2}-\sum _{i=1}^{N}w_{i}^{2}}}\cdot \sum _{i=1}^{N}{\frac {w_{i}(x_{i}-{\overline {x}}^{*})^{2}}{(\sigma _{x_{i}})^{2}}}.} 306: 3080:
Lance P. Black, Sandra L. Kamo, Charlotte M. Allen, John N. Aleinikoff, Donald W. Davis, Russell J. Korsch, Chris Foudoulis 2003. TEMORA 1: a new zircon standard for Phanerozoic Uโ€“Pb geochronology. Chemical Geology 200,
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MSWD < 1 if the observed scatter is less than that predicted by the analytical uncertainties. In this case, the data are said to be "underdispersed", indicating that the analytical uncertainties were overestimated.
2318: 461: 1040: 540: 1271:{\displaystyle \sigma ^{2}={\frac {\sum _{i=1}^{N}(x_{i}-{\overline {x}})^{2}}{N}}{\text{ and }}s^{2}={\frac {N}{N-1}}\cdot \sigma ^{2}={\frac {1}{N-1}}\cdot \sum _{i=1}^{N}(x_{i}-{\overline {x}})^{2}.} 205: 2306:{\displaystyle s^{2}={\frac {\sum _{i=1}^{N}w_{i}x_{i}^{2}\cdot \sum _{i=1}^{N}w_{i}-{\big (}\sum _{i=1}^{N}w_{i}x_{i}{\big )}^{2}}{{\big (}\sum _{i=1}^{N}w_{i}{\big )}^{2}-\sum _{i=1}^{N}w_{i}^{2}}}.} 1408: 840:, the MSWD is a measure of goodness of fit that takes into account the relative importance of both the internal and external reproducibility, with most common usage in isotopic dating. 586: 2749:, the reduced chi-squared statistic is called the outfit mean-square statistic, and the information-weighted reduced chi-squared statistic is called the infit mean-square statistic. 1782:{\displaystyle \sigma ^{2}={\frac {\sum _{i=1}^{N}w_{i}x_{i}^{2}\cdot \sum _{i=1}^{N}w_{i}-{\big (}\sum _{i=1}^{N}w_{i}x_{i}{\big )}^{2}}{{\big (}\sum _{i=1}^{N}w_{i}{\big )}^{2}}}.} 1286: 807: 717: 679: 2026:{\displaystyle s^{2}={\frac {\sum _{i=1}^{N}w_{i}}{{\big (}\sum _{i=1}^{N}w_{i}{\big )}^{2}-\sum _{i=1}^{N}w_{i}^{2}}}\cdot {\sum _{i=1}^{N}w_{i}(x_{i}-{\overline {x}}^{*})^{2}}.} 749: 625: 963: 341: 2915: 381: 54: 214: 929: 902: 3155: 769: 401: 3037: 3025: 3015: 972: 489: 3150: 1283:
When individual determinations of an age are not of equal significance, it is better to use a weighted mean to obtain an "average" age, as follows:
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reasons have been proposed to explain the overdispersion of (U-Th)/He data, including unevenly distributed U-Th distributions and radiation damage.
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indicates that the fit has not fully captured the data (or that the error variance has been underestimated). In principle, a value of
3060: 3052: 2895: 2870: 2816: 2789: 72: 2449:{\displaystyle {\text{MSWD}}_{u}={\frac {1}{N-1}}\cdot \sum _{i=1}^{N}{\frac {(x_{i}-{\overline {x}})^{2}}{\sigma _{x_{i}}^{2}}}.} 544: 3111:, Jon Woodhead 2002. Improving isochron calculations with robust statistics and the bootstrap. Chemical Geology 185, 191โ€“204. 2924: 2768:
Wendt, I., and Carl, C., 1991, The statistical distribution of the mean squared weighted deviation, Chemical Geology, 275โ€“285.
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McDougall, I. and Harrison, T. M. 1988. Geochronology and Thermochronology by the Ar/Ar Method. Oxford University Press.
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When each measured value can be assumed to have the same weighting, or significance, the biased and unbiased (or "
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Often the geochronologist will determine a series of age measurements on a single sample, with the measured value
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indicates that the extent of the match between observations and estimates is in accord with the error variance. A
476: 1544:{\displaystyle \sigma ^{2}={\frac {\sum _{i=1}^{N}w_{i}(x_{i}-{\overline {x}}^{*})^{2}}{\sum _{i=1}^{N}w_{i}}},} 817: 3003:
Measurements and Their Uncertainties: A Practical Guide to Modern Error Analysis, By Ifan Hughes, Thomas Hase
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age) space, or if the compositional data fit a bivariate normal distribution in -space (for the central age).
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How Bad is Good? A Critical Look at the Fitting of Reflectivity Models using the Reduced Chi-Square Statistic
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By analogy, the weighted mean square of the weighted deviations (weighted MSWD) can be computed as follows:
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The unweighted mean square of the weighted deviations (unweighted MSWD) can then be computed, as follows:
483: 395: 208: 133: 114: 813:" the data: either the model is improperly fitting noise, or the error variance has been overestimated. 722: 598: 934: 314: 2036:
The unbiased weighted estimator of the sample variance can also be computed on the fly as follows:
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Dickin, A. P. 1995. Radiogenic Isotope Geology. Cambridge University Press, Cambridge, UK, 1995,
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but this value can be misleading, unless each determination of the age is of equal significance.
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is the weight matrix, the inverse of the input (diagonal) covariance matrix of observations. If
3056: 3048: 2891: 2866: 2812: 2806: 2785: 2779: 1396:{\displaystyle {\overline {x}}^{*}={\frac {\sum _{i=1}^{N}w_{i}x_{i}}{\sum _{i=1}^{N}w_{i}}}.} 354: 17: 3092: 907: 880: 855: 106: 94: 2831: 863: 754: 3144: 1049:" and "population" respectively) estimators of the variance are computed as follows: 837: 2964: 1791:
The unbiased weighted estimator of the sample variance can be computed as follows:
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Again, the corresponding standard deviation is the square root of the variance.
810: 301:{\displaystyle \chi ^{2}=\sum _{i}{\frac {(O_{i}-C_{i})^{2}}{\sigma _{i}^{2}}}} 3096: 86: 3036:
Computational Methods in Physics and Engineering, By Samuel Shaw Ming Wong
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Dealing with Uncertainties: A Guide to Error Analysis, By Manfred Drosg
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As a general rule, when the variance of the measurement error is known
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then one might weight the first measurement twice that of the second.
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When the variance of the measurement error is only partially known,
456:{\displaystyle \chi _{\nu }^{2}={\frac {r^{\mathrm {T} }Wr}{\nu }},} 3026:
Practical Statistics for Astronomers, By J. V. Wall, C. R. Jenkins
1035:{\displaystyle {\overline {x}}={\frac {\sum _{i=1}^{N}x_{i}}{N}},} 535:{\displaystyle \chi _{\nu }^{2}={\frac {\mathrm {RSS} }{\nu }},} 3123:"What do Infit and Outfit, Mean-square and Standardized mean?" 29: 1405:
The biased weighted estimator of variance can be shown to be
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Parameter Estimation and Hypothesis Testing in Linear Models
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the reduced chi-squared may serve as a correction estimated
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Data Reduction and Error Analysis for the Physical Sciences
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The standard deviation is the square root of the variance.
200:{\displaystyle \chi _{\nu }^{2}={\frac {\chi ^{2}}{\nu }},} 398:, the definition is often written in matrix notation as 50: 2464: 2321: 2042: 1797: 1557: 1411: 1289: 1055: 975: 937: 910: 883: 777: 757: 725: 687: 649: 601: 547: 492: 404: 357: 317: 217: 158: 207:where the chi-squared is a weighted sum of squared 45:
may be too technical for most readers to understand
2730: 2448: 2305: 2025: 1781: 1543: 1395: 1270: 1034: 957: 923: 896: 801: 763: 743: 711: 673: 619: 580: 534: 455: 375: 335: 300: 199: 969:The arithmetic mean of the age determinations is 134:Ordinary least squares ยง Reduced chi-squared 3091:Journal of the Geological Society 166, 919โ€“932 2923:, University California, Davis, archived from 2811:. Springer Berlin Heidelberg. Section 3.2.5. 2557: 2518: 2247: 2208: 2193: 2144: 1888: 1849: 1762: 1723: 1708: 1659: 8: 2984: 2982: 595:When the fit is just an ordinary mean, then 2784:. Wellesley-Cambridge Press. p. 301. 581:{\displaystyle \mathrm {RSS} =\sum r^{2},} 2863:Standard Mathematical Tables and Formulae 2716: 2704: 2699: 2684: 2674: 2664: 2654: 2641: 2634: 2628: 2617: 2601: 2596: 2586: 2575: 2562: 2556: 2555: 2548: 2538: 2527: 2517: 2516: 2508: 2498: 2487: 2480: 2471: 2466: 2463: 2435: 2428: 2423: 2412: 2398: 2389: 2379: 2373: 2362: 2337: 2328: 2323: 2320: 2291: 2286: 2276: 2265: 2252: 2246: 2245: 2238: 2228: 2217: 2207: 2206: 2198: 2192: 2191: 2184: 2174: 2164: 2153: 2143: 2142: 2133: 2123: 2112: 2099: 2094: 2084: 2074: 2063: 2056: 2047: 2041: 2013: 2003: 1993: 1983: 1970: 1960: 1949: 1944: 1932: 1927: 1917: 1906: 1893: 1887: 1886: 1879: 1869: 1858: 1848: 1847: 1839: 1829: 1818: 1811: 1802: 1796: 1767: 1761: 1760: 1753: 1743: 1732: 1722: 1721: 1713: 1707: 1706: 1699: 1689: 1679: 1668: 1658: 1657: 1648: 1638: 1627: 1614: 1609: 1599: 1589: 1578: 1571: 1562: 1556: 1529: 1519: 1508: 1496: 1486: 1476: 1466: 1453: 1443: 1432: 1425: 1416: 1410: 1381: 1371: 1360: 1348: 1338: 1328: 1317: 1310: 1301: 1291: 1288: 1259: 1245: 1236: 1223: 1212: 1187: 1178: 1153: 1144: 1135: 1123: 1109: 1100: 1087: 1076: 1069: 1060: 1054: 1017: 1007: 996: 989: 976: 974: 947: 942: 936: 915: 909: 888: 882: 787: 782: 776: 756: 735: 730: 724: 697: 692: 686: 659: 654: 648: 611: 606: 600: 569: 548: 546: 513: 511: 502: 497: 491: 431: 430: 423: 414: 409: 403: 356: 327: 322: 316: 290: 285: 274: 264: 251: 241: 235: 222: 216: 183: 177: 168: 163: 157: 73:Learn how and when to remove this message 57:, without removing the technical details. 2952:, University Science Books, p. 268 2764: 2762: 2758: 2914:Laub, Charlie; Kuhl, Tonya L. (n.d.), 2909: 2907: 2834:Practical Regression and Anova using R 387:minus the number of fitted parameters 2865:. Chapman&Hall/CRC. p. 626. 802:{\displaystyle \chi _{\nu }^{2}<1} 712:{\displaystyle \chi _{\nu }^{2}>1} 674:{\displaystyle \chi _{\nu }^{2}\gg 1} 55:make it understandable to non-experts 7: 3156:Statistical deviation and dispersion 2778:Strang, Gilbert; Borre, Kae (1997). 383:, equals the number of observations 2846:Kenney, J.; Keeping, E. S. (1963). 555: 552: 549: 520: 517: 514: 432: 25: 2950:An introduction to error analysis 2781:Linear algebra, geodesy, and GPS 744:{\displaystyle \chi _{\nu }^{2}} 620:{\displaystyle \chi _{\nu }^{2}} 486:, the definition simplifies to: 467:is the vector of residuals, and 126:standard error of the regression 34: 3151:Geochronological dating methods 958:{\displaystyle \sigma _{x_{i}}} 846:MSWD = 1 if the age data fit a 336:{\displaystyle \sigma _{i}^{2}} 99:mean squared weighted deviation 3127:Rasch Measurement Transactions 2890:. Princeton University Press. 2745:In data analysis based on the 2713: 2692: 2681: 2647: 2409: 2382: 2010: 1976: 1493: 1459: 1256: 1229: 1120: 1093: 848:univariate normal distribution 681:indicates a poor model fit. A 271: 244: 130:standard error of the equation 18:Mean square weighted deviation 1: 2989:Bevington, Philip R. (1969), 809:indicates that the model is " 97:testing. It is also known as 2948:Taylor, John Robert (1997), 2850:. van Nostrand. p. 187. 2669: 2403: 1998: 1481: 1296: 1250: 1114: 981: 91:reduced chi-square statistic 588:where the numerator is the 3172: 2805:Koch, Karl-Rudolf (2013). 120:Its square root is called 3097:10.1144/0016-76492008-117 2848:Mathematics of Statistics 1551:which can be computed as 477:generalized least squares 351:. The degree of freedom, 122:regression standard error 2966:Chi-Square Curve Fitting 931:and an associated error 376:{\displaystyle \nu =n-m} 3121:Linacre, J. M. (2002). 2993:, New York: McGraw-Hill 2963:Kirkman, T. W. (n.d.), 2886:Hayashi, Fumio (2000). 2861:Zwillinger, D. (1995). 2832:Julian Faraway (2000), 590:residual sum of squares 111:variance of unit weight 93:is used extensively in 2732: 2633: 2591: 2543: 2503: 2450: 2378: 2307: 2281: 2233: 2169: 2128: 2079: 2027: 1965: 1922: 1874: 1834: 1783: 1748: 1684: 1643: 1594: 1545: 1524: 1448: 1397: 1376: 1333: 1272: 1228: 1092: 1036: 1012: 959: 925: 898: 803: 765: 745: 713: 675: 621: 582: 536: 484:ordinary least squares 475:is non-diagonal, then 457: 396:weighted least squares 377: 347:, and calculated data 337: 302: 201: 115:weighted least squares 2733: 2613: 2571: 2523: 2483: 2451: 2358: 2308: 2261: 2213: 2149: 2108: 2059: 2028: 1945: 1902: 1854: 1814: 1784: 1728: 1664: 1623: 1574: 1546: 1504: 1428: 1398: 1356: 1313: 1273: 1208: 1072: 1037: 992: 960: 926: 924:{\displaystyle w_{i}} 899: 897:{\displaystyle x_{i}} 804: 766: 746: 714: 676: 622: 583: 537: 458: 378: 338: 303: 202: 2462: 2319: 2040: 1795: 1555: 1409: 1287: 1053: 973: 935: 908: 881: 775: 755: 723: 685: 647: 599: 545: 490: 402: 355: 315: 215: 156: 2606: 2440: 2296: 2104: 1937: 1619: 904:having a weighting 792: 740: 702: 664: 616: 507: 419: 332: 295: 173: 2728: 2592: 2446: 2419: 2303: 2282: 2090: 2023: 1923: 1779: 1605: 1541: 1393: 1268: 1032: 955: 921: 894: 799: 778: 761: 741: 726: 709: 688: 671: 650: 629:standard deviation 627:equals the sample 617: 602: 578: 532: 493: 453: 405: 373: 333: 318: 298: 281: 240: 197: 159: 113:in the context of 2930:on 6 October 2016 2723: 2672: 2608: 2469: 2441: 2406: 2353: 2326: 2298: 2001: 1939: 1774: 1536: 1484: 1388: 1299: 1253: 1203: 1169: 1138: 1133: 1117: 1027: 984: 843:In general when: 764:{\displaystyle 1} 527: 448: 296: 231: 192: 150:degree of freedom 144:It is defined as 83: 82: 75: 16:(Redirected from 3163: 3135: 3134: 3118: 3112: 3105: 3099: 3088: 3082: 3078: 3072: 3069: 3063: 3045: 3039: 3034: 3028: 3023: 3017: 3012: 3006: 3001: 2995: 2994: 2986: 2977: 2976: 2975: 2973: 2960: 2954: 2953: 2945: 2939: 2938: 2937: 2935: 2929: 2922: 2911: 2902: 2901: 2883: 2877: 2876: 2858: 2852: 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2712: 2700: 2695: 2691: 2680: 2663: 2650: 2637: 2636: 2554: 2544: 2515: 2504: 2482: 2465: 2460: 2459: 2424: 2408: 2385: 2381: 2342: 2322: 2317: 2316: 2244: 2234: 2205: 2190: 2180: 2170: 2129: 2080: 2058: 2043: 2038: 2037: 2009: 1992: 1979: 1966: 1885: 1875: 1846: 1835: 1813: 1798: 1793: 1792: 1759: 1749: 1720: 1705: 1695: 1685: 1644: 1595: 1573: 1558: 1553: 1552: 1525: 1503: 1492: 1475: 1462: 1449: 1427: 1412: 1407: 1406: 1377: 1355: 1344: 1334: 1312: 1290: 1285: 1284: 1255: 1232: 1192: 1174: 1158: 1140: 1137: and  1119: 1096: 1071: 1056: 1051: 1050: 1013: 991: 971: 970: 943: 938: 933: 932: 911: 906: 905: 884: 879: 878: 856:arithmetic mean 834: 829: 773: 772: 753: 752: 721: 720: 683: 682: 645: 644: 637: 597: 596: 565: 543: 542: 488: 487: 426: 425: 400: 399: 353: 352: 343:, observations 313: 312: 270: 260: 247: 243: 218: 213: 212: 179: 154: 153: 142: 107:isotopic dating 95:goodness of fit 79: 68: 62: 59: 51:help improve it 48: 39: 35: 28: 23: 22: 15: 12: 11: 5: 3169: 3167: 3159: 3158: 3153: 3143: 3142: 3137: 3136: 3113: 3107:Roger Powell, 3100: 3083: 3073: 3064: 3040: 3029: 3018: 3007: 2996: 2978: 2955: 2940: 2903: 2896: 2878: 2871: 2853: 2838: 2824: 2817: 2797: 2790: 2770: 2757: 2756: 2754: 2751: 2742: 2741:Rasch analysis 2739: 2727: 2719: 2715: 2707: 2703: 2698: 2694: 2687: 2683: 2677: 2671: 2668: 2662: 2657: 2653: 2649: 2644: 2640: 2631: 2626: 2623: 2620: 2616: 2612: 2604: 2599: 2595: 2589: 2584: 2581: 2578: 2574: 2570: 2565: 2559: 2551: 2547: 2541: 2536: 2533: 2530: 2526: 2520: 2511: 2507: 2501: 2496: 2493: 2490: 2486: 2479: 2474: 2445: 2438: 2431: 2427: 2422: 2415: 2411: 2405: 2402: 2397: 2392: 2388: 2384: 2376: 2371: 2368: 2365: 2361: 2357: 2351: 2348: 2345: 2341: 2336: 2331: 2302: 2294: 2289: 2285: 2279: 2274: 2271: 2268: 2264: 2260: 2255: 2249: 2241: 2237: 2231: 2226: 2223: 2220: 2216: 2210: 2201: 2195: 2187: 2183: 2177: 2173: 2167: 2162: 2159: 2156: 2152: 2146: 2141: 2136: 2132: 2126: 2121: 2118: 2115: 2111: 2107: 2102: 2097: 2093: 2087: 2083: 2077: 2072: 2069: 2066: 2062: 2055: 2050: 2046: 2022: 2016: 2012: 2006: 2000: 1997: 1991: 1986: 1982: 1978: 1973: 1969: 1963: 1958: 1955: 1952: 1948: 1943: 1935: 1930: 1926: 1920: 1915: 1912: 1909: 1905: 1901: 1896: 1890: 1882: 1878: 1872: 1867: 1864: 1861: 1857: 1851: 1842: 1838: 1832: 1827: 1824: 1821: 1817: 1810: 1805: 1801: 1778: 1770: 1764: 1756: 1752: 1746: 1741: 1738: 1735: 1731: 1725: 1716: 1710: 1702: 1698: 1692: 1688: 1682: 1677: 1674: 1671: 1667: 1661: 1656: 1651: 1647: 1641: 1636: 1633: 1630: 1626: 1622: 1617: 1612: 1608: 1602: 1598: 1592: 1587: 1584: 1581: 1577: 1570: 1565: 1561: 1540: 1532: 1528: 1522: 1517: 1514: 1511: 1507: 1499: 1495: 1489: 1483: 1480: 1474: 1469: 1465: 1461: 1456: 1452: 1446: 1441: 1438: 1435: 1431: 1424: 1419: 1415: 1392: 1384: 1380: 1374: 1369: 1366: 1363: 1359: 1351: 1347: 1341: 1337: 1331: 1326: 1323: 1320: 1316: 1309: 1304: 1298: 1295: 1267: 1262: 1258: 1252: 1249: 1244: 1239: 1235: 1231: 1226: 1221: 1218: 1215: 1211: 1207: 1201: 1198: 1195: 1191: 1186: 1181: 1177: 1173: 1167: 1164: 1161: 1157: 1152: 1147: 1143: 1132: 1126: 1122: 1116: 1113: 1108: 1103: 1099: 1095: 1090: 1085: 1082: 1079: 1075: 1068: 1063: 1059: 1031: 1026: 1020: 1016: 1010: 1005: 1002: 999: 995: 988: 983: 980: 950: 946: 941: 918: 914: 891: 887: 864:geometric mean 833: 830: 828: 825: 798: 795: 790: 785: 781: 760: 738: 733: 729: 708: 705: 700: 695: 691: 670: 667: 662: 657: 653: 636: 633: 614: 609: 605: 577: 572: 568: 564: 561: 557: 554: 551: 531: 526: 522: 519: 516: 510: 505: 500: 496: 452: 447: 443: 440: 434: 429: 422: 417: 412: 408: 372: 369: 366: 363: 360: 330: 325: 321: 293: 288: 284: 277: 273: 267: 263: 259: 254: 250: 246: 238: 234: 230: 225: 221: 196: 191: 186: 182: 176: 171: 166: 162: 141: 138: 81: 80: 42: 40: 33: 27:Test statistic 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 3168: 3157: 3154: 3152: 3149: 3148: 3146: 3132: 3128: 3124: 3117: 3114: 3110: 3104: 3101: 3098: 3094: 3087: 3084: 3077: 3074: 3068: 3065: 3062: 3061:0-521-59891-5 3058: 3054: 3053:0-521-43151-4 3050: 3044: 3041: 3038: 3033: 3030: 3027: 3022: 3019: 3016: 3011: 3008: 3005: 3000: 2997: 2992: 2985: 2983: 2979: 2968: 2967: 2959: 2956: 2951: 2944: 2941: 2926: 2919: 2918: 2910: 2908: 2904: 2899: 2897:0-691-01018-8 2893: 2889: 2882: 2879: 2874: 2872:0-8493-2479-3 2868: 2864: 2857: 2854: 2849: 2842: 2839: 2836: 2835: 2828: 2825: 2820: 2818:9783662039762 2814: 2810: 2809: 2801: 2798: 2793: 2791:9780961408862 2787: 2783: 2782: 2774: 2771: 2765: 2763: 2759: 2752: 2750: 2748: 2740: 2738: 2725: 2717: 2705: 2701: 2696: 2685: 2675: 2666: 2660: 2655: 2651: 2642: 2638: 2629: 2624: 2621: 2618: 2614: 2610: 2602: 2597: 2593: 2587: 2582: 2579: 2576: 2572: 2568: 2563: 2549: 2545: 2539: 2534: 2531: 2528: 2524: 2509: 2505: 2499: 2494: 2491: 2488: 2484: 2477: 2472: 2456: 2443: 2436: 2429: 2425: 2420: 2413: 2400: 2395: 2390: 2386: 2374: 2369: 2366: 2363: 2359: 2355: 2349: 2346: 2343: 2339: 2334: 2329: 2313: 2300: 2292: 2287: 2283: 2277: 2272: 2269: 2266: 2262: 2258: 2253: 2239: 2235: 2229: 2224: 2221: 2218: 2214: 2199: 2185: 2181: 2175: 2171: 2165: 2160: 2157: 2154: 2150: 2139: 2134: 2130: 2124: 2119: 2116: 2113: 2109: 2105: 2100: 2095: 2091: 2085: 2081: 2075: 2070: 2067: 2064: 2060: 2053: 2048: 2044: 2034: 2020: 2014: 2004: 1995: 1989: 1984: 1980: 1971: 1967: 1961: 1956: 1953: 1950: 1946: 1941: 1933: 1928: 1924: 1918: 1913: 1910: 1907: 1903: 1899: 1894: 1880: 1876: 1870: 1865: 1862: 1859: 1855: 1840: 1836: 1830: 1825: 1822: 1819: 1815: 1808: 1803: 1799: 1789: 1776: 1768: 1754: 1750: 1744: 1739: 1736: 1733: 1729: 1714: 1700: 1696: 1690: 1686: 1680: 1675: 1672: 1669: 1665: 1654: 1649: 1645: 1639: 1634: 1631: 1628: 1624: 1620: 1615: 1610: 1606: 1600: 1596: 1590: 1585: 1582: 1579: 1575: 1568: 1563: 1559: 1538: 1530: 1526: 1520: 1515: 1512: 1509: 1505: 1497: 1487: 1478: 1472: 1467: 1463: 1454: 1450: 1444: 1439: 1436: 1433: 1429: 1422: 1417: 1413: 1403: 1390: 1382: 1378: 1372: 1367: 1364: 1361: 1357: 1349: 1345: 1339: 1335: 1329: 1324: 1321: 1318: 1314: 1307: 1302: 1293: 1281: 1278: 1265: 1260: 1247: 1242: 1237: 1233: 1224: 1219: 1216: 1213: 1209: 1205: 1199: 1196: 1193: 1189: 1184: 1179: 1175: 1171: 1165: 1162: 1159: 1155: 1150: 1145: 1141: 1130: 1124: 1111: 1106: 1101: 1097: 1088: 1083: 1080: 1077: 1073: 1066: 1061: 1057: 1048: 1043: 1029: 1024: 1018: 1014: 1008: 1003: 1000: 997: 993: 986: 978: 967: 948: 944: 939: 916: 912: 889: 885: 875: 871: 867: 865: 861: 857: 853: 849: 844: 841: 839: 838:geochronology 832:Geochronology 831: 826: 824: 822: 821: 814: 812: 796: 793: 788: 783: 779: 758: 736: 731: 727: 706: 703: 698: 693: 689: 668: 665: 660: 655: 651: 642: 634: 632: 630: 612: 607: 603: 593: 591: 575: 570: 566: 562: 559: 529: 524: 508: 503: 498: 494: 485: 480: 478: 474: 470: 466: 450: 445: 441: 438: 427: 420: 415: 410: 406: 397: 392: 390: 386: 370: 367: 364: 361: 358: 350: 346: 328: 323: 319: 311: 308:with inputs: 291: 286: 282: 275: 265: 261: 257: 252: 248: 236: 232: 228: 223: 219: 210: 194: 189: 184: 180: 174: 169: 164: 160: 151: 147: 139: 137: 135: 131: 127: 123: 118: 116: 112: 108: 104: 100: 96: 92: 88: 77: 74: 66: 56: 52: 46: 43:This article 41: 32: 31: 19: 3130: 3126: 3116: 3103: 3086: 3076: 3067: 3043: 3032: 3021: 3010: 2999: 2990: 2970:, retrieved 2965: 2958: 2949: 2943: 2932:, retrieved 2925:the original 2916: 2888:Econometrics 2887: 2881: 2862: 2856: 2847: 2841: 2833: 2827: 2807: 2800: 2780: 2773: 2744: 2457: 2314: 2035: 1790: 1404: 1282: 1279: 1044: 968: 876: 872: 868: 859: 858:age) or log( 851: 845: 842: 835: 827:Applications 820:a posteriori 819: 815: 640: 638: 594: 481: 472: 468: 464: 393: 388: 384: 348: 344: 143: 129: 125: 121: 119: 110: 102: 98: 90: 84: 69: 60: 44: 3109:Janet Hergt 2747:Rasch model 862:) (for the 811:overfitting 3145:Categories 2753:References 635:Discussion 209:deviations 146:chi-square 140:Definition 87:statistics 63:April 2021 3133:(2): 878. 2697:σ 2676:∗ 2670:¯ 2661:− 2615:∑ 2611:⋅ 2573:∑ 2569:− 2525:∑ 2485:∑ 2421:σ 2404:¯ 2396:− 2360:∑ 2356:⋅ 2347:− 2263:∑ 2259:− 2215:∑ 2151:∑ 2140:− 2110:∑ 2106:⋅ 2061:∑ 2005:∗ 1999:¯ 1990:− 1947:∑ 1942:⋅ 1904:∑ 1900:− 1856:∑ 1816:∑ 1730:∑ 1666:∑ 1655:− 1625:∑ 1621:⋅ 1576:∑ 1560:σ 1506:∑ 1488:∗ 1482:¯ 1473:− 1430:∑ 1414:σ 1358:∑ 1315:∑ 1303:∗ 1297:¯ 1251:¯ 1243:− 1210:∑ 1206:⋅ 1197:− 1176:σ 1172:⋅ 1163:− 1115:¯ 1107:− 1074:∑ 1058:σ 994:∑ 982:¯ 940:σ 854:(for the 784:ν 780:χ 732:ν 728:χ 694:ν 690:χ 666:≫ 656:ν 652:χ 608:ν 604:χ 563:∑ 525:ν 499:ν 495:χ 479:applies. 446:ν 411:ν 407:χ 368:− 359:ν 320:σ 283:σ 258:− 233:∑ 220:χ 190:ν 181:χ 165:ν 161:χ 3081:155โ€“170. 751:around 641:a priori 310:variance 592:(RSS). 49:Please 3059:  3051:  2972:30 May 2934:30 May 2894:  2869:  2815:  2788:  1047:sample 463:where 89:, the 2928:(PDF) 2921:(PDF) 132:(see 128:, or 105:) in 3057:ISBN 3049:ISBN 2974:2015 2936:2015 2892:ISBN 2867:ISBN 2813:ISBN 2786:ISBN 2468:MSWD 2325:MSWD 794:< 704:> 643:, a 148:per 109:and 103:MSWD 3093:doi 850:in 836:In 482:In 394:In 85:In 53:to 3147:: 3131:16 3129:. 3125:. 3055:, 2981:^ 2906:^ 2761:^ 823:. 631:. 391:. 211:: 152:: 136:) 124:, 117:. 3095:: 2900:. 2875:. 2821:. 2794:. 2726:. 2718:2 2714:) 2706:i 2702:x 2693:( 2686:2 2682:) 2667:x 2656:i 2652:x 2648:( 2643:i 2639:w 2630:N 2625:1 2622:= 2619:i 2603:2 2598:i 2594:w 2588:N 2583:1 2580:= 2577:i 2564:2 2558:) 2550:i 2546:w 2540:N 2535:1 2532:= 2529:i 2519:( 2510:i 2506:w 2500:N 2495:1 2492:= 2489:i 2478:= 2473:w 2444:. 2437:2 2430:i 2426:x 2414:2 2410:) 2401:x 2391:i 2387:x 2383:( 2375:N 2370:1 2367:= 2364:i 2350:1 2344:N 2340:1 2335:= 2330:u 2301:. 2293:2 2288:i 2284:w 2278:N 2273:1 2270:= 2267:i 2254:2 2248:) 2240:i 2236:w 2230:N 2225:1 2222:= 2219:i 2209:( 2200:2 2194:) 2186:i 2182:x 2176:i 2172:w 2166:N 2161:1 2158:= 2155:i 2145:( 2135:i 2131:w 2125:N 2120:1 2117:= 2114:i 2101:2 2096:i 2092:x 2086:i 2082:w 2076:N 2071:1 2068:= 2065:i 2054:= 2049:2 2045:s 2021:. 2015:2 2011:) 1996:x 1985:i 1981:x 1977:( 1972:i 1968:w 1962:N 1957:1 1954:= 1951:i 1934:2 1929:i 1925:w 1919:N 1914:1 1911:= 1908:i 1895:2 1889:) 1881:i 1877:w 1871:N 1866:1 1863:= 1860:i 1850:( 1841:i 1837:w 1831:N 1826:1 1823:= 1820:i 1809:= 1804:2 1800:s 1777:. 1769:2 1763:) 1755:i 1751:w 1745:N 1740:1 1737:= 1734:i 1724:( 1715:2 1709:) 1701:i 1697:x 1691:i 1687:w 1681:N 1676:1 1673:= 1670:i 1660:( 1650:i 1646:w 1640:N 1635:1 1632:= 1629:i 1616:2 1611:i 1607:x 1601:i 1597:w 1591:N 1586:1 1583:= 1580:i 1569:= 1564:2 1539:, 1531:i 1527:w 1521:N 1516:1 1513:= 1510:i 1498:2 1494:) 1479:x 1468:i 1464:x 1460:( 1455:i 1451:w 1445:N 1440:1 1437:= 1434:i 1423:= 1418:2 1391:. 1383:i 1379:w 1373:N 1368:1 1365:= 1362:i 1350:i 1346:x 1340:i 1336:w 1330:N 1325:1 1322:= 1319:i 1308:= 1294:x 1266:. 1261:2 1257:) 1248:x 1238:i 1234:x 1230:( 1225:N 1220:1 1217:= 1214:i 1200:1 1194:N 1190:1 1185:= 1180:2 1166:1 1160:N 1156:N 1151:= 1146:2 1142:s 1131:N 1125:2 1121:) 1112:x 1102:i 1098:x 1094:( 1089:N 1084:1 1081:= 1078:i 1067:= 1062:2 1030:, 1025:N 1019:i 1015:x 1009:N 1004:1 1001:= 998:i 987:= 979:x 949:i 945:x 917:i 913:w 890:i 886:x 860:t 852:t 797:1 789:2 759:1 737:2 707:1 699:2 669:1 661:2 613:2 576:, 571:2 567:r 560:= 556:S 553:S 550:R 530:, 521:S 518:S 515:R 509:= 504:2 473:W 469:W 465:r 451:, 442:r 439:W 433:T 428:r 421:= 416:2 389:m 385:n 371:m 365:n 362:= 349:C 345:O 329:2 324:i 292:2 287:i 276:2 272:) 266:i 262:C 253:i 249:O 245:( 237:i 229:= 224:2 195:, 185:2 175:= 170:2 101:( 76:) 70:( 65:) 61:( 47:. 20:)

Index

Mean square weighted deviation
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make it understandable to non-experts
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statistics
goodness of fit
isotopic dating
weighted least squares
Ordinary least squares ยง Reduced chi-squared
chi-square
degree of freedom
deviations
variance
weighted least squares
generalized least squares
ordinary least squares
residual sum of squares
standard deviation
overfitting
the reduced chi-squared may serve as a correction estimated a posteriori
geochronology
univariate normal distribution
arithmetic mean
geometric mean
sample
Rasch model


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