Organizational Performance and Entrepreneurial Orientation: The Intervening Role of Organizational Learning

Many past studies have examined the association between entrepreneurial orientation (E.O.) and organizational performance (O.P.). However, these studies have not adequately addressed the mediating roles of acquisition learning (A.L.) and experiential learning (E.L.) on organizational performance. Given this gap, we have developed a new model that contains six direct relationships, three mediating relationships, and one multi-mediating relationship. The focus of the study was on Indonesian Pharmaceutical SMEs. We have collected a sample of 365 respondents non-randomly. For statistical analysis, we have used Smart PLS version 3.2. The statistical analysis includes reliability, validity, and descriptive statistics. The results confirm that acquisition learning (A.L.), experiential learning (E.L.), and entrepreneurial orientation (E.O.) promote organizational performance (O.P.). We also found that entrepreneurial orientation (E.O.) impacts acquisition learning (A.L.) and innovative performance (I.P.) but does not affect organizational performance (O.P.). However, the results suggest that acquisition learning (A.L.) and experiential learning (E.L.) are positively linked. Our results also support all the mediating relationships

3,4-Dimethyl-2-(2-oxo-2-phenyl­eth­yl)-2H,4H-pyrazolo­[4,3-c][1,2]benzothia­zine-5,5-dione

In the title mol­ecule, C19H17N3O3S, the heterocyclic thia­zine ring adopts a half-chair conformation with the S and N atoms displaced by 0.530 (5) and 0.229 (6) Å, respectively, on opposite sides of the mean plane formed by the remaining ring atoms. The ethanone group lies at an angle of 3.8 (3)° with respect to the benzene ring, which lies almost perendicular to the pyrazole ring, with a dihedral between the two planes of 89.22 (11)°. Weak inter­molecular C—H⋯O hydrogen-bonding inter­actions are present

2-(3,4-Dimethyl-5,5-dioxo-2H,4H-pyrazolo[4,3-c][1,2]benzothia­zin-2-yl)-N′-(2-thienylmethyl­idene)acetohydrazide

In the title mol­ecule, C18H17N5O3S2, the heterocyclic thia­zine ring adopts a twist boat conformation, with the S and N atoms displaced by 0.480 (7) and 0.205 (8) Å, respectively, on opposite sides of the mean plane formed by the remaining ring atoms. The pyrazole and benzene rings are tilted at an angle of 10.9 (2)° with respect to one another. The crystal structure is stabilized by inter­molecular N—H⋯O and C—H⋯N hydrogen bonds, resulting in dimers forming nine-membered rings of graph-set motif R 2 2(9). In addition, inter­molecular C—H⋯O inter­actions result in chains of mol­ecules along the c axis, further consolidating the crystal packing

2-(3,4-Dimethyl-5,5-dioxo-2H,4H-pyrazolo­[4,3-c][1,2]benzothia­zin-2-yl)-1-(4-meth­oxy­phen­yl)ethanone

In the title mol­ecule, C20H19N3O4S, the heterocyclic thia­zine ring adopts a half-chair conformation with the S and N atoms displaced by 0.492 (6) and 0.199 (6) Å, respectively, on opposite sides from the mean plane formed by the remaining ring atoms. The ethanone group lies at an angle of 9.4 (2)° with respect to the benzene ring, which lies almost perpendicular to the pyrazole ring, with a dihedral between the two planes of 78.07 (9)°. In the crystal, mol­ecules are linked by weak C—H⋯O hydrogen bonds

Application of model based post-stack inversion in the characterization of reservoir sands containing porous, tight and mixed facies: a case study from the Central Indus Basin, Pakistan

Porosity is a key parameter for reservoir evaluation. Inferring the porosity from seismic data is often challenging and prone to uncertainties due to number of factors. The main aim of this paper is to show the applicability of seismic inversion on old vintage seismic data to map spatial porosity at reservoir level. 3D-seismic and wireline log data are used to map the reservoir properties of the Lower Goru productive sands in the Gambat Latif block, Central Indus Basin, Pakistan. The Lower Goru formation was interpreted with the help of seismic and well data. Interpreted horizons are thus further used in model-based seismic inversion techniques to map the spatial distribution of porosity. Well-log data are used in the construction of low acoustic impedance models. Calibration of reservoir porosity with inverted acoustic impedance is achieved through well-log data. The results from model-based inversion reasonably estimate the porosity distribution within the C-sand interval of the Lower Goru Member. After post-stack inversion, the porosity values at wells Tajjal-01, Tajjal-02 and Tajjal-03 are 10%, 8% and 12%, respectively. Porosity values calculated from post-stack inversion at the corresponding well locations are in good agreement with the borehole-derived porosity