It overcame the shortcoming of the hardthreshold function's discontinuousness and improves the constant error.

该阈值函数既克服了硬阈值函数不的缺点,又修正了软阈值函数存在的恒定偏差。

Catastrophe theory has become a useful tool in studying incontinuous phenomena since it was established.

摘要突变理论自问世以来已成为研究实世界中一些不象的有力工具。

Ichnofabric analysis displays a rising significance on accurate environmental interpretation of sedimentary units in oil-bearing basin and precise recognition of depositional disconuities.

近来，遗迹组构分析增长的意义主要表在含油气盆地地层单元成因环境的精确解释和各类不面的精细识别。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不的内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

It overcame the shortcoming of the hardthreshold function's discontinuousness and improves the constant error.

该数既克服了硬数不连续的缺点,又修正了软数存在的恒定偏差。

Catastrophe theory has become a useful tool in studying incontinuous phenomena since it was established.

摘要突变理论自问世以来已成为研究现实世界中一些不连续现象的有力工具。

Ichnofabric analysis displays a rising significance on accurate environmental interpretation of sedimentary units in oil-bearing basin and precise recognition of depositional disconuities.

近来，遗迹组构分析其日益增长的意义主要表现在含油气盆地地层单元成因环境的精确解释和各类不连续面的精细识别。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不连续的后地质体,通常赋存于断裂带、角砾岩体岩层(岩性单位)中。

It overcame the shortcoming of the hardthreshold function's discontinuousness and improves the constant error.

该阈值函数既克服了硬阈值函数不连续的缺点,又修正了软阈值函数存在的恒定偏差。

Catastrophe theory has become a useful tool in studying incontinuous phenomena since it was established.

摘要突变理论自问世以已成为研究现实世界中一些不连续现象的有力。

Ichnofabric analysis displays a rising significance on accurate environmental interpretation of sedimentary units in oil-bearing basin and precise recognition of depositional disconuities.

，组构分析其日益增长的意义主要表现在含油气盆地地层单元成因环境的精确解释和各类不连续面的精细识别。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

It overcame the shortcoming of the hardthreshold function's discontinuousness and improves the constant error.

该阈值函数既克服了硬阈值函数不连续缺点,又修正了软阈值函数恒定偏差。

Catastrophe theory has become a useful tool in studying incontinuous phenomena since it was established.

摘要突变理论自问世以来已成为研究现实世界中一些不连续现象有力工具。

Ichnofabric analysis displays a rising significance on accurate environmental interpretation of sedimentary units in oil-bearing basin and precise recognition of depositional disconuities.

近来，遗迹组构分析其日益增长意义主要表现含油气盆地地层单元成因环境精确解释不连续面精细识别。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床矿体是一些不连续内生或后生地质体,通常赋于断裂带、角砾岩体或岩层(岩性单位)中。

It overcame the shortcoming of the hardthreshold function's discontinuousness and improves the constant error.

该数既克服了硬数不的缺点,又修正了软数存在的恒定偏差。

Catastrophe theory has become a useful tool in studying incontinuous phenomena since it was established.

摘要突变理论自问世以来已成为研究现实世界中一些不现象的有力工具。

Ichnofabric analysis displays a rising significance on accurate environmental interpretation of sedimentary units in oil-bearing basin and precise recognition of depositional disconuities.

近来，遗迹组构分析其日益增长的意义主要表现在含油气盆地地层单元成因环境的精确解释和各类不的精细识别。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不的内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

It overcame the shortcoming of the hardthreshold function's discontinuousness and improves the constant error.

该阈值函数既克服了硬阈值函数不连续的缺点,又修正了软阈值函数存在的恒。

Catastrophe theory has become a useful tool in studying incontinuous phenomena since it was established.

摘要突变理论自问世以来已成为研究现实世界中一些不连续现象的有力工具。

Ichnofabric analysis displays a rising significance on accurate environmental interpretation of sedimentary units in oil-bearing basin and precise recognition of depositional disconuities.

近来，遗迹组构分析其日益增长的意义主要表现在含油气盆地地层单元成因环境的释和各类不连续面的细识别。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

It overcame the shortcoming of the hardthreshold function's discontinuousness and improves the constant error.

该阈值函数既克服了硬阈值函数不连续的缺点,又修正了软阈值函数存在的恒定偏差。

Catastrophe theory has become a useful tool in studying incontinuous phenomena since it was established.

摘要突变理论自问世以来研究现实世界中一些不连续现象的有力工具。

Ichnofabric analysis displays a rising significance on accurate environmental interpretation of sedimentary units in oil-bearing basin and precise recognition of depositional disconuities.

近来，遗迹组构分析其日益增长的意义主要表现在盆地地层单元因环境的精确解释和各类不连续面的精细识别。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

It overcame the shortcoming of the hardthreshold function's discontinuousness and improves the constant error.

该阈值函数既克服了硬阈值函数不连续的缺点,又修正了软阈值函数存在的恒定偏差。

Catastrophe theory has become a useful tool in studying incontinuous phenomena since it was established.

摘突变理论自问以来已成为研究现中一些不连续现象的有力工具。

Ichnofabric analysis displays a rising significance on accurate environmental interpretation of sedimentary units in oil-bearing basin and precise recognition of depositional disconuities.

近来，遗迹组构分析其日益增长的意表现在含油气盆地地层单元成因环境的精确解释和各类不连续面的精细识别。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床的矿体是一些不连续的内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

It overcame the shortcoming of the hardthreshold function's discontinuousness and improves the constant error.

该阈值函数既克服了硬阈值函数不连续缺点,又修正了软阈值函数存在恒定。

Catastrophe theory has become a useful tool in studying incontinuous phenomena since it was established.

要突变理论自问世以来已成为研究现实世界中一些不连续现象有力工具。

Ichnofabric analysis displays a rising significance on accurate environmental interpretation of sedimentary units in oil-bearing basin and precise recognition of depositional disconuities.

近来，遗迹组构分析其日益增长意义主要表现在含油气盆地地层单元成因环境解释和各类不连续面细识别。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积岩金矿床矿体是一些不连续内生或后生地质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。