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.

该函数既克服了硬函数不连续缺点,又修正了软函数存在恒定偏差。

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地地层单元成因环境的精确解释和各类不连续面的精细。

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.

积岩金矿床的矿体是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)。

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。

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.

摘要突变理论自问世以来已成为研究现实世界中一些续现象的有力工具。

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

该阈值函既克服了硬阈值函续的缺点,又修正了软阈值函存在的恒定偏差。

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地地层单元成因环境的精确解释和各类续面的精细识别。

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.

摘要突变理论自问世以来已成为研究现实世界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地地层单元成因环境的精确解释和各类不连续面的精。

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)。

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.

该阈值函既克服了硬阈值函不连续的缺点,又修正了软阈值函的恒定偏差。

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，遗迹组构分益增长的意义主要表现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来已成为研究实世界中一些有力工具。

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在含油气盆地地层单元成因环境精确解释和各类面精细识别。

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地地层单元成因环境的精确解释和各类不连续面的精细。

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.

积岩金矿床的矿体是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)。