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。

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在的恒定偏差。

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内生或后生地质体,通常赋裂带、角砾岩体或岩层(岩性单位)中。

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。

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

该阈值克服了硬阈值不连续缺点,又修正了软阈值存在恒定偏差。

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精确解释和各类不连续面精细识别。

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,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

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。

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。

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和各类不连续面精细识别。

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。

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为研究现实世界中一些不连续现象的有力工具。

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。

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

近，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.

沉积岩金床的一些不连续的内生或后生地质,通常赋存于断裂带、角砾岩或岩层(岩性单位)中。

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的有力工具。

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。

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或质体,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

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

摘要突变问世以来已成为研究现实世界中一些不现象有力工具。

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缺点,又修正了软阈值函数存在恒定偏差。

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精确解释和各类不面精细识别。

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。

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。

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定偏差。

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和各类不连续面精细识别。

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,通常赋存于断裂带、角砾岩体或岩层(岩性单位)中。

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。

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在的恒定偏差。

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内生或后生地质体,通于断裂带、角砾岩体或岩层(岩性单位)中。

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工具。

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。

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

，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。

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

摘要突变问世以来已成为研究现实世界中一些不现象有力工具。

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缺点,又修正了软阈值函数存在恒定偏差。

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精确解释和各类不面精细识别。

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。