車籠埔斷層深鑽岩心鏡煤素反射率研究

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車籠埔斷層深鑽岩心鏡煤素反射率研究

梁珪宏 , Masters　　Advisor：蔡龍珆　　

繁體中文

鏡煤素反射率；車籠埔斷層； none

Abstract │ Reference (94) │ Altmetrics

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ABSTRACT
The 1999. 9.21 Chi-Chi earthquake, triggered by Chelungpu Fault, led to a tremendous life and property loss in Taiwan, also aroused the attention to tectonic structures and fault activity. The plant remains in sedimentary strata gradually decompose and rearrange their organic molecules after deep burial, diagenesis, and tectonic activities. In other words, the plant macerals turn to be more matured out of the increasing temperature and pressure during thermal maturation. Furthermore, the maturation process is irreversible, not influenced by retrograde metamorphism, can only record the maximum thermal event in the burial history. Vitrinite reflectance had been proved to reflect this thermal/pressure information successfully.
The drilling work of TCDP (Taiwan Chelungpu-fault Drilling Project) core was completed on December, 2004. Core over 1500m in length was successfully recovered from –500m down to –2000m. Black carbonaceous materials were collected from this core for the purpose of evaluating thermal mechanism in the well site, especially at the fracture zones of Chelungpu Fault. The purpose of this study is to evaluate the thermal mechanism of fault zone by vitrinite reflectance. According to the study result, there is no obvious increase of vitrinite reflectance from surface to the depth of 2000m in TCDP core. It can be attributed to the reasons of 1) Chelungpu Fault did not deep-cut the strata to produce enough heat, or 2) sample positions were not close enough to the fault position.

Reference ( 94 ) 〈TOP〉

Antia, D. D. J., 1986, Kinetic method for modeling vitrinite reflectance: Geology, Vol. 14, p. 606-608.
連結：
Barker, C. E. and Elders, W. A., 1981, Vitrinite reflectance geothermonetry and apparent heating duration in the Cerro Prito geothermal field. Geothermics, No. 10, p. 207-223.
連結：
Barker, C. E. and Goldstein, R. H., 1990, Fluid-inclusion technique for determining maximum temperature in calcite and its comparison to the vitrinite reflectancd geothermometer, Geology, Vol. 18, p. 1003-1006.
連結：
Barker, C. E. and Pawlewicz, M. J., 1986, The correlation of vitrinite reflectance with maximum temperature in humic organic matter: in Buntebarthm, G., and Stegena, L. (eds.) Paleogeothermics, New York, Springer-Verlag, p. 79-93.
連結：
Barr, T. D. and Dahlen, F. A., 1990, Constraints on friction and stress in the Taiwan fold and thrust belt from heat flow and geochronology: Geology, Vol. 18, p. 111-115.
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