Triton-triton correlation functions have been measured for^(40)Ar+^(197)Au collisions at E/A=25 MeV.The anticorrelations at small relative momenta are observed and become more pronounced with the increasing total ener...Triton-triton correlation functions have been measured for^(40)Ar+^(197)Au collisions at E/A=25 MeV.The anticorrelations at small relative momenta are observed and become more pronounced with the increasing total energy of two coincident tritons.Comparison with the three-body trajectory calculations indicates that the average emission times lie between 100 and 300fm/c for tritons.展开更多
In order to determine the tectonic framework of the Late Paleozoic sedimentary basin of the studied area in Inner Mongolia, horizontal derivative, vertical derivative, total gradient modulus, tilt angle, and Euler dec...In order to determine the tectonic framework of the Late Paleozoic sedimentary basin of the studied area in Inner Mongolia, horizontal derivative, vertical derivative, total gradient modulus, tilt angle, and Euler deconvolution methods were used to process the high-precision gravity data. Four major faults and six secondary faults have been identified according to the horizontal fault position information provided by the first four methods, and the fault depth information were obtained using the Euler deconvolution method. The interpreted faults were identified as the main basin-controlling structures in the study area, which was helpful for deepening the understanding of the basin's structure, as well as providing important references for delineating hidden polymetallic ore veins.展开更多
基金Supported by the National Natural Science Foundation of Chinathe Science Foundation of the Chinese Academy of Science.
文摘Triton-triton correlation functions have been measured for^(40)Ar+^(197)Au collisions at E/A=25 MeV.The anticorrelations at small relative momenta are observed and become more pronounced with the increasing total energy of two coincident tritons.Comparison with the three-body trajectory calculations indicates that the average emission times lie between 100 and 300fm/c for tritons.
文摘In order to determine the tectonic framework of the Late Paleozoic sedimentary basin of the studied area in Inner Mongolia, horizontal derivative, vertical derivative, total gradient modulus, tilt angle, and Euler deconvolution methods were used to process the high-precision gravity data. Four major faults and six secondary faults have been identified according to the horizontal fault position information provided by the first four methods, and the fault depth information were obtained using the Euler deconvolution method. The interpreted faults were identified as the main basin-controlling structures in the study area, which was helpful for deepening the understanding of the basin's structure, as well as providing important references for delineating hidden polymetallic ore veins.
